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At PLAY, we have a mind, body, spirit approach to health and well-being. We believe peace, love and yoga are essential to living a healthy life. For us, peace is about connecting with the quiet, calm nature within and that feeling of being at home. Love is positive emotion. Yoga is the culmination of peace and love through moving meditation guided by your breath. Sharing peace and love through kindness and compassion with others brings community together at PLAY studio.
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Play Turned 6 and We Celebrated
We want to send a special thank you out to our beautiful community of yogis who celebrated with us. You all have helped to make Play the inspiring place to practice that it is for the last 6 years. We so appreciate everyone who took the time to come by share the love, meet with […]
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Anatomy of Inversions with Sarah Haughton
July 23 from 1:30-3:30
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The power of the gospel: Can black churches survive turbulent times?
When the Legislature tried to do away with affirmative action last year, Davis invited the politicians to Calvary Baptist to have a discussion with his congregation. The passion and determination in the room was palpable.
"We will continue to try to giving the poor and the voiceless power," Davis said. "That's what we believe the Bible teaches us is right."
Calvary sponsors many programs designed to uplift not only the African American community, but also to help build bridges with the rest of society. The church sponsors subsidized housing for the elderly and disabled. Only a handful of the residents in Calvary Tower, the church's low-income housing complex, are congregation members.
"I trust two people in this world," said 78-year-old Patsy Moore, who is able to maintain her independence because Calvary rents her an apartment for a mere $275 a month. "That's my eldest son and Pastor Davis."
Every Sunday morning, members team up with believers from a local predominately-Hispanic church to feed the homeless at Pioneer Park.
As volunteers dish up chili and hot dogs, biscuits and traditional Mexican soup, a recording of Calvary's distinctive choir plays in the background. A line snakes through the trees and around the playground, where some have stowed their clothing and bedding underneath the slide for safekeeping.
"They're my family," says one volunteer, Mary Daniels, 63, of her fellow believers at Calvary Baptist Church.
Says another man, a non-believer with black leather skin and gnarled yellow nails, tapping his cane against the sidewalk, "I don't have much use for church. I don't need the food. I come here every Sunday because of my people. The black people. My people are here."
Member, nonmember, black, white, brown — Calvary Baptist doesn't care.
Davis prays for them all.
EMAIL: firstname.lastname@example.com, TWITTER: elizMstuart
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Nov 09, 2004
BAGHDAD [MENL] -- Iraq and the United States, launching a long-expected airand ground offensive, have completed the first phase of the operation tocapture Faluja.
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CAIRO [MENL] -- The Palestinian Authority was said to have cooperated in anEgyptian investigation of a series of car bombings against tourist targetsin the Sinai Peninsula.


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University of Cambridge > Talks.cam > Institute of Astronomy Galaxies Discussion Group > The Lyman break analogue Haro 11: spatially resolved chemodynamics with VLT FLAMES
The Lyman break analogue Haro 11: spatially resolved chemodynamics with VLT FLAMES
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Comments about 'Utah football: Brian Johnson officially leaves Utah for Mississippi State'
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- Newest first
- Most recommended
Good for Brian. He finally bets to be a part of a winning program. Best of luck to him.
- 4:43 p.m. Feb. 10, 2014
- Like (2)
- Report abuse
Thanks for your contributions to the program both as a player and a coach. We will never forget your MVP performance in the Sugar Bowl! Best of luck in your new adventure.
- 4:51 p.m. Feb. 10, 2014
- Like (6)
- Report abuse
BJ is a class act as a player, coach, and a person. I like to think we will see him again one day on the Utah sideline. Best of luck to you, Brian!
- 4:54 p.m. Feb. 10, 2014
- Like (6)
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Best of luck to BJ. I hope he does well.
SEC rules that was hilarious. Max Hall might be #2 candidate
- 5:25 p.m. Feb. 10, 2014
- Like (1)
- Report abuse
Good luck BJ and Roll the Tide!
- 6:42 p.m. Feb. 10, 2014
- Like (5)
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Smart move to get out before the pink slips are handed out in December.
Good luck and may success be found in Mississippi.
- 9:16 p.m. Feb. 10, 2014
- Like (2)
- Report abuse
Great move - timing is everything.
- 11:58 p.m. Feb. 10, 2014
- Like (2)
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It's a good time to leave before Whitt's last season.
- 9:31 a.m. Feb. 11, 2014
- Like (2)
- Report abuse
BJ, GOOD LUCK! You are a class act. Thanks for your work in the community as
well as at the U.
The bad news - you are going to the SEC. Frying pan and fire. Yes, MSU went 7-6 but they had three cupcake wins against Bowling Green, Troy, and Alcorn State. They struggled to beat Arkansas, Kentucky and Ole Miss. They could just as easily have finished at 5-7 (sound familiar?) Tennessee and Florida will both be better. MSU won't finish higher than 5th out of 8 teams in the SEC West and 10th out of 14 overall. The coaching staff there is also on the hot seat. A bad year will see them all canned.
MSU has a talented, but erratic sophomore (again, sound familiar?) QB in Dak Prescott. They did NOT recuit a QB this year. There is no clear choice for back-up. I'm not sure this position was a step up. Give it your best shot!
Go Gators!
- 11:35 a.m. Feb. 11, 2014
- Like (1)
- Report abuse
I wish Brian all the best at Mississippi State. I am disappointed to see him
go. I think he is a great position coach and has become one of the Utes better
recruiters the last few years.
Brian has a great young football mind and I hope to see him back on the Utes sidelines someday.
I just hope Kyle doesn't look down south for his replacement. The coaching staff has way too many of his inner circle former cougars. I hear they are looking at the QB coach from Wake Forrest. I don't know much about him, but that would be a refreshing change.
- 4:11 p.m. Feb. 11, 2014
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Reviews - Sutcliffe Hotel2
70 72, Albert Road, Blackpool, FY1 4PR
Price FromView Rooms
Customer Reviews
Our reviews are from genuine LateRooms.com customers. We verify that the customer has stayed before leaving a review.
100% would recommend it to a friend
Customer service
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Sutcliffe hotel blackpool
Stayed for 1 night and the hotel was great Check in was quick and easy and we were greeted with a smile Room was very clean just a little small Enjoyed the bar at the hotel and very reasonabley priced Breakfast was lovely Definitely we will be going back.
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Thank you for your review and I can only apologise for next doors kitchen extractor.
good food and very good staff
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Mom Who "Gifted" Daughter Remains In Jail After Judge Denies Bail Reduction Pennsylvania woman charged in connection with 12 girls found in a Feasterville home has been denied bail reduction.
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You are here > Home > Baseball Newsstand > Baseball Primer Newsblog > Discussion
Baseball Primer Newsblog
— The Best News Links from the Baseball Newsstand
Thursday, December 29, 2011
Images of 2011: Caption This! Ichiro and Jack Wilson
Caption this image:
Creative Commons by Keith Allison
Gamingboy Posted: December 29, 2011 at 03:25 PM | 22 comment(s) Login to Bookmark
Tags: community, special topics
Reader Comments and Retorts
Statements posted here are those of our readers and do not represent the BaseballThinkFactory. Names are provided by the poster and are not verified. We ask that posters follow our submission policy. Please report any inappropriate comments.1. Best Regards, President of Comfort, Esq. Posted: December 29, 2011 at 03:38 PM (#4025054)
The Seattle Ballet's performance of #6org closed after the second act.2. Wins Above Paul Westerberg Posted: December 29, 2011 at 03:45 PM (#4025060)
Trust fall?3. villageidiom Posted: December 29, 2011 at 03:49 PM (#4025062)
Ichiro could've fielded it, if he wanted to.4. Rickey! [quote], not [code] Posted: December 29, 2011 at 03:51 PM (#4025064)
Send that guy to Atlanta before he kills Ichiro!5. Gonfalon Bubble Posted: December 29, 2011 at 03:54 PM (#4025071)
Boy, boy, crazy boy, keep cooly-cool, boy!6. Dale Sams Posted: December 29, 2011 at 04:07 PM (#4025080)
?????????????????7. UCCF Posted: December 29, 2011 at 04:23 PM (#4025093)
Dude, I sure hope that's dirt on the seat of your pants.8. KJOK Posted: December 29, 2011 at 08:21 PM (#4025346)
Sorry, didn't know I could throw you that far!9. Jefferson Manship (Dan Lee) Posted: December 29, 2011 at 08:30 PM (#4025352)
Do not want.10. Guapo Posted: December 29, 2011 at 08:49 PM (#4025368)
backup infielder11. Walt Davis Posted: December 29, 2011 at 08:57 PM (#4025377)
diving for routine popup
I need a new team.
Is that even legal?12. Gonfalon Bubble Posted: December 29, 2011 at 09:02 PM (#4025380)
13. Walt Davis Posted: December 29, 2011 at 09:04 PM (#4025382)
On an annoying note:14. Guapo Posted: December 29, 2011 at 09:46 PM (#4025409)
That looks like a very odd play. I see the warning track but no foul line so this must be in foul territory.
Fine, foul pop down the RF line often sees the RF and 2B going after it but the 2B would be going after it with his back towards 2B and headed towards the warning track but that's not the direction Wilson is heading. Ichiro too would be headed towards the stand at a more extreme angle whereas he seems to be coming almost straight in.
I suppose if it was a reasonably high pop-up but a crazy windy day Wilson might have gotten there but then had to leap back at the last second.
Or is that a basepath and this is some bizarre play where Wilson is coming out from SS and Ichiro is coming in from RF and the 2B and CF are cracking up yelling "you got it! you got it!"?
#1 wins the caption contest.
15. Walt Davis Posted: December 30, 2011 at 12:05 AM (#4025492)
Thanks for the vid. Apparently foul lines are just invisible from that angle. Fair territory, Wilson over-ran the ball in the direction of the foul line (maybe windy) and had to dive back.16. zfan Posted: December 30, 2011 at 03:33 AM (#4025578)
Look out, we got a badass over here!17. There's a bustle in Misirlou's hedgerow Posted: December 30, 2011 at 03:38 AM (#4025579)
Thanks for the vid. Apparently foul lines are just invisible from that angle.
Not invisible, just not in the picture. Pause the vid at around 37 sec, and you'll see that the dirt track extends into fair territory. That's what we see in the photo, the portion of the dirt track in fair territory.
"NOOOOOOOOOOOOO!!"19. Shoeless Swedish Chef Posted: December 30, 2011 at 03:13 PM (#4025716)
"In my next trick I will levitate an infielder"20. Ray (RDP) Posted: December 30, 2011 at 06:55 PM (#4025889)
In light of Greg Spira's passing I was reading some of his old posts on rec.sport.baseball and came across this post of his re Tony Gwynn from November 1993. It struck me because it sounds similar in many respects to the current Ichiro discussion (specifically, whether his defense as judged by some of the metrics at the time was really great enough to carry his not-very-special offense).21. Ray (RDP) Posted: December 30, 2011 at 07:17 PM (#4025900)
I didn't want to post it in Greg's thread because I didn't want to detract from the remembrances of him there, so I'll just post it here.
I recall that there was a time in the early 90s that people thought Gwynn was overrated and wasn't a Hall of Famer. But the way he finished his career -- with strong hitting despite durability issues -- moved him to a solid middle-tier HOFer.
His discussion of fielding runs below sounds a bit like the current discussions re WAR's defensive ratings.
Greg wrote:
A lot of TP's high rating of Gwynn is based on his really high number of fielding runs. As you probably know, most people here are quite skeptical of fielding runs. If the fielding runs listed for Gwynn are indeed accurate assesments of his defensive value, then I think most
Comparing Gwynn through 1993 with Ichiro through 2010 (let's leave out Ichiro's terrible 2011, and actually doing that makes their games played equal) is interesting:22. Walt Davis Posted: December 31, 2011 at 12:47 AM (#4026046)
Gwynn thru 1993:
1585 G, 6828 PA, 129 OPS+, 50 WAR (43 oWar; 8 dWAR)
Rbat 246, Rbaser 29, RRoe 2, Rdp 7m Rfld 69, Rpos -69
Ichiro thru 2010:
1588 G, 7339 PA, 117 OPS+, 55 WAR (42 oWAR; 13 dWAR)
Rbat 159, Rbaser 48, RRoe 4, Rdp 44, Rfld 132, Rpos -68
Ichiro's steals and (according to WAR) his baserunning brings him even with Gwynn in offense (see oWAR). Greg was worried that Gwynn's defense was being over-evaluated, and per WAR Gwynn's defense was indeed very good; Ichiro's is off the charts.
Gwynn went on in his next year, 1994, to hit for a 169 OPS+, but because of the strike he only got 110 games in, so his WAR was only 3.4. Ichiro in his next year, 2011, had a horrible season in virtually all respects, finishing with a -0.4 WAR.
This puts the two players virtually even in WAR after 1994/2011. Of course, Gwynn was "only" 35 at that point and had a very good finish to his career, posting 15 more WAR despite his durability issues, which made him an easy HOFer, while Ichiro will be trying to show in 2012 at age 38 that his age 37 performance was mainly a fluke and not the onset of serious decline. Not shown above is a comparison of peak/prime, but what keeps Ichiro even with Gwynn, at least according to WAR, is baserunning and defense calculations that are off the charts.
Extending to Carew through 1978:
1635 G, 6980 PA, 137 OPS+, 62.7 WAR (61.7 oWAR)
Rbat 323, Rbaser 34, Rroe -1, Rdp 15, Rfield 10, Rpos -1
Better hitter in a lower-scoring era -- I assume he crushes them on peak, he was nearly Morgan at his peak although that's also when the switch to 1B occurred -- and most of the rest is positional adjustment vs. Rfield.
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سكس نيك بنات ورجال The show isn`t entirely without its strengths of course. The driver`s prediction is called the dial-in and is posted on the race car. سكس فيديو مص ونيك Amazingly, this year we are also sharing not only the first name, but both of us are also driving mustangs, and both cars will also rock a similar paint scheme. سكس فلاحي Have your partner lay on the sofa, then slowly stick your tongue out on their navel. سكس فيديو مص ونيك Kirby gave Paul and Linda specially drawn illustration after learning of Macca`s tune `Magneto and Titanium Man,` which was inspired by Kirby`s Marvel Comics creations. Being one of the most contrasting countries in Southeast Asia, how does Malaysia turn several influencies into indigenous habits, how does it link back to its cultural roots? It`s been a while since we`ve seen you on PSP, Naruto -- and it looks like you`ve grown up. Hot and Cold Kiss - Lick your partner`s lips so that they`re warm, and then gently blow on them.
} : The time it takes a drag-race vehicle to travel from the starting line to the finish line. سكس نيك بنات ورجال The piston in a racing engine has a large diameter for the engine size, and it goes up and down a relatively short distance on each cycle.
This means that a race car engine can run much faster -- up to 15,000 RPM in a Champ Car engine -- but has relatively little torque. I never recorded them, but remembered a few jokes here and there that always made me laugh. سكس فيديو مص ونيك The pitch might originate at an anime studio {like the ones named in the question}.


text:
|Publication number
|Publication type
|Application number
|Publication date
|Apr 15, 1997
|Filing date
|Sep 10, 1996
|Priority date
|Jan 18, 1994
|Fee status
|Publication number
|Thomas G. Harris, Donald L. Luffel, Joseph M. Hawkins
|Original Assignee
|Restech, Inc.
|Export Citation
|BiBTeX, EndNote, RefMan
|Patent Citations (1), Non-Patent Citations (8), Referenced by (25), Classifications (8), Legal Events (3)
|External Links: USPTO, USPTO Assignment, Espacenet
This application is a continuation of application Ser. No. 08/592,608 filed on Jan. 26, 1996 now abandoned which was a continuation of application Ser. No. 08/182,450 filed on Jan. 18, 1994 now abandoned.
This invention relates to a global method for predicting the hydrocarbon/water level for oil and gas wells, and more particularly to such a method which predicts such level from routine log data derived parameters of porosity, water saturation, and air permeability.
When exploring for or developing new oil and gas reservoirs, the borehole of a well high on a structure may not penetrate the hydrocarbon/water contact. This contact level should be determined to locate delineation wells, plan development drilling, and forecast reserves and economics, especially when operating in high-cost areas.
In principal, hydrocarbon/water levels can be predicted from a combination of capillary pressure data, and log or core derived porosity φ, water saturation Sw, and air permeability k. The J-curve correlation presented in a paper by M. C. Leverett entitled "Capillary Behavior in Porous Solids" published in Trans AIME, Vol. 142, pp 151-69, 1941, was developed for unconsolidated sand packs, and was the earliest method proposed to relate laboratory data of capillary pressure Pc, water saturation Sw, porosity φ and air permeability k.
Later R. P. Alger, et al. in a paper entitled "New Unified Method of Integrating Core Capillary Pressure Data with Well Logs" and published by SPEFE, pp 145-52 in June 1989 employed a multilinear regression approach to relate these same properties to both core and log data. More recently, D. Smith in an article entitled "How to Predict Down-Dip Water Level" published in World Oil, pp 85-88 in May 1992 predicted the water level from logs with a method for generating synthetic mercury capillary pressure Pc curves if no actual capillary pressure Pc data are available.
The above methods have had only limited success for several reasons. First, laboratory measured capillary pressure data specific to the reservoir are usually not available. Second, to describe the entire reservoir, great care is required for integrating the laboratory capillary pressure data from a few core measurements with log data. Further, if the wells in the reservoir are high above the transition zone, a small error in water saturation produces a large error in the predicted water table. Thus, prior methods are highly sensitive to certain errors that can result in large errors in the predicted water level.
It is an object of the present invention to provide a method for predicting the hydrocarbon/water contact level in an oil or gas well that may be utilized in the absence of any laboratory data.
A further object of the invention is to provide such a method which simplifies the integration of capillary pressure data Pc with log and core data, and minimizes the error in predicting the hydrocarbon/water contact level in a stratigraphic zone which contains hydrocarbons.
The method of the present invention is based on a capillary pressure model that relates four quantities: (1) porosity, (2) water saturation, (3) air permeability, and (4) capillary pressure. In the absence of any laboratory capillary pressure Pc data, the model utilizes worldwide correlations from large diverse data bases obtained from sources such as Shell Oil Co. and Amoco Corporation.
The hydrocarbon/water level of a hydrocarbon bearing zone is predicted through regression analysis using porosity φ and water saturation Sw from log and/or core analysis. As a result of the regression analysis, an error range may be assigned to the predicted water level. As well known, regression is a measure of the extent to which two variables increase together, or the extent to which one variable increases as the other decreases. The regression analysis locates the hydrocarbon/water level that best utilizes all available log and core data in a reservoir. Regression improves the resolution of the prediction by averaging down errors and identifies the error range bounding the predicted water level. The error range is established with a 95% confidence level which means that 95 times out of 100, the actual water level is between the upper and lower limits predicted.
In the regression approach applied, all observed variables are considered to have associated errors. In this case, the observed variables are derived from well log or core analysis information results. At each depth level, there are four observed variables: depth, porosity, water saturation, and air permeability. Although some or all of the last three values may be calculated from logs rather than measured on cores, for the sake of simplicity these values are treated as observations subject to random error. The sum of the weighted squares of these errors is minimized, constrained by derived equations relating the observed values. Thus, more accurate error ranges may be predicted with regression analysis for the determination of hydrocarbon/water contact level.
FIG. 1 is a graphical representation of a hyperbolic curve for capillary pressure data in accord with an equation developed by J. H. M. Thomeer;
FIG. 2 is a graphical representation of the correlation between permeabilities and mercury capillary pressures developed by B. F. Swanson and related to point A on the curve of FIG. 1;
FIG. 3 is a graphical representation of the relation between pore-throat radius at point A of FIG. 1 and air permeability developed by E. D. Pittman;
FIG. 4 is a graphical correlation between measured capillary pressure data and capillary pressure data calculated in accord with the present invention;
FIG. 5 is a representation of a log of a clean gas sand in an Indonesian well;
FIG. 6 is a graphical correlation between water saturations calculated from the present invention compared against measured water saturation from five cores of the Indonesian well illustrated in FIG. 5; and
FIG. 7 is the representation of a log in a well offshore of the Ivory Coast, Africa.
The advanced capillary pressure method of the present invention utilizes parameters and equations of others in obtaining the model equations utilized in the present invention.
One of these equations was presented in an article by J. H. M. Thomeer entitled "Introduction of a Pore Geometrical Factor Defined by the Capillary Pressure Curve" published by JPT in March 1960, pp 73-77. This article proposed that mercury capillary pressure data be mathematically modelled as hyperbolic curves using the following equation: ##EQU2##
where Sb.spsb.∞ is percentage bulk volume of rock occupied by mercury at infinite pressure, Sb is percentage bulk volume occupied by mercury, Fg is a pore geometrical factor, Pc is mercury capillary pressure (psi), and Pd is mercury displacement pressure (psi). However, if it is assumed that Sb.spsb.∞ is proportional to rock porosity and Sb is proportional to rock porosity times hydrocarbon saturation, then equation (1) may be rewritten in more familiar terms as follows:
log Pc =-Fg /In (1-Sw)+log Pd, (2)
where Sw is water saturation.
The simplified equation (2) above adequately represents capillary pressure data, except in complex rocks, where microporosity creates double-humped curves.
An article by B. F. Swanson entitled "A Simple Correlation Between Permeabilities And Mercury Capillary Pressures" published in JPT, December 1981, pp 2,498-2,504, shows that the coordinates from a special point A on the capillary pressure curve developed from equation 1 and illustrated in FIG. 1 of the drawings is related to the permeability of the rock to air, or "air permeability". This relationship is described in the following equation: ##EQU3##
where ka is air permeability, φ is porosity of the rock, Sw is water saturation and Pc is mercury capillary pressure with SwA representing water saturation at point A on the curve of FIG. 1 and Pc.sbsb.A representing capillary pressure at point A of the curve shown in FIG. 1. FIG. 2 illustrates the correlation between ka and Sb.sbsb.a =φ(1-Sw)A.
The pore geometrical factor, Fg, and mercury displacement pressure Pd can be determined from knowledge of water saturation Sw at point A of FIG. 1 and capillary pressure Pc at point A through the relations of equations (4) and (5):
Fg =[In (1-Sw)A ]2 /2.303 (4)
Pd =Pc.sbsb.A (1-Sw)A (5)
The equations (4) and (5), with that of equation (2) are sufficient to determine the capillary pressure curve of FIG. 1. In other words, information as to the porosity, PcA and SwA is sufficient to define the capillary pressure curve of equation (2).
Equations 4 and 5 show that knowledge of the porosity φ, the capillary pressure at point A of the curve, PcA, and the water saturation at point A of the curve, SwA, is sufficient to determine the capillary pressure curve of FIG. 1 from equation 2 above.
It is necessary to determine Pc.sbsb.A and SwA in order to obtain the capillary pressure as indicated by the application of equation (2) above. In an article by E. D. Pittman entitled "Relationship of Porosity and Permeability to Various Parameters Derived from Mercury Injection Capillary Pressure Curves for Sandstone" in the AAPG Bulletin, Vol. 42, No. 2, published February 1992, pp 191-198, an equation as set forth below shows a relationship between the pore-throat radius at Point A on FIG. 1 and air permeability in sandstone.
log rapex =-0.226+0.4666 log ka, (6)
where rapex is the pore-throat radius at point A and ka is air permeability. The relationship set forth in equation (6) was established using multiple regression on data from two hundred and two (202) samples of sandstone from fourteen (14) formations ranging in age from Ordovician to Tertiary.
The porosities ranged from 3.30 percent to 28 percent, and the permeabilities ranged from 0.05 md to 998 md. The correlation between the calculated pore-throat radius at point A rapex and the observed pore-throat radius is illustrated by the graph in FIG. 3. The capillary pressure Pc at point A on the curve of FIG. 1 may be calculated by converting the pore-throat radius at point A, rapex, to mercury capillary pressure Pc by the following equation:
Pc =107/rapex (7)
The water saturation Sw may be calculated for point A in terms of porosity φ and air permeability ka by first calculating the capillary pressure Pc from air permeability ka by the following equation:
Pc =180/ka 0.466. (8)
Then the capillary pressure calculated from equation (8) above may be substituted in equation (3) above to determine the water saturation Sw at point A in terms of porosity and permeability. Equation (3) as set forth above is: ##EQU4##
The pore geometrical factor Fg was calculated for equation (4) above and the following equation (9) for pore geometrical factor Fg is derived from equation (4): ##EQU5##
Likewise, the mercury displacement pressure Pd was calculated in equation (5) above and the following equation (10) for the mercury displacement pressure Pd is derived from equation (5):
Pd =937.8/(ka 0.3406)φ. (10)
The four quantities of porosity φ, water saturation Sw, air permeability ka, and capillary pressure Pc have now been related through the several equations (1) through (10) set forth above. The relationship of equations (2), (9), and (10) have been specifically identified for the present invention.
As a relatively large number of core data bases are utilized in the derivation of the capillary pressure curves, a worldwide correlation has been provided. When measured laboratory data is not available, the model derived from the several equations above may be used to provide capillary pressure curves characterizing a reservoir.
As illustrated in FIG. 4, three capillary pressure curves derived by the above equations are illustrated for different porosities and permeabilities indicated. The points on the graph of FIG. 4 are plotted from measured capillary pressure data from a Miocene sandstone formation. A very close comparison is obtained in the first curve having a high permeability. The model may be improved from actual capillary pressure data to adjust the constants in equations (9) and (10) as the data becomes available.
For determining, the free-water level or height in a well, the present method is applied to well data, and laboratory capillary pressures are converted to height h above the free-water level by equation (11) as follows: ##EQU6##
In equation 11,
pw =formation water density
ph =formation hydrocarbon density
σr =interfacial tension between the fluids in the reservoir
σi =interfacial tension for mercury in the laboratory
θr =contact angle between water and reservoir rock
θi =contact angle between mercury and rock in laboratory
The reservoir fluid interfacial tension values are usually not measured but must be obtained form correlations as developed by others. For example, see an article of T. T. Schowalter entitled "Mechanics of Secondary Hydrocarbon Migration and Entrapment" AAPQ Bulletin, Vol. 36, No. 5, published May 1979 pp 723-760.
The model developed by the method of this invention permits the estimation of an error range in the predicted height h of the free-water level. This estimation is based on regression which is a measure of the extent that two variables increase together or of the extent to which one increases as the other decreases. All of the observed variables are considered to have associated errors resulting from logs or core analysis. At each depth level, the four observed variables are (1) depth, (2) porosity, (3) water saturation, and (4) air permeability. All values are treated as observations even though some of the values may be calculated from logs. The equations utilized by the model relating to the observed values constrain or minimize this error.
As a result of regression, error bars or upper and lower estimated water levels are provided as computed by a chi-square distribution using 95% confidence limits. For a large number of trials, the actual water level should be between the upper and lower confidence limits 95 times out of 100. Typical error bars are shown on Table 1 below in which all values are measured in terms of distance below the lowest known hydrocarbon.
TABLE 1______________________________________TYPICAL ERROR BARS FOR FREE-WATERLEVEL PREDICTIONSDistance below lowest known oilPredicted Upper Lowerfree-water level, ft. confidence limit, ft. confidence limit, ft.______________________________________10 6 17100 60 170______________________________________
The resolution of the method is improved if the logged pay interval contains the transition zone rather than being high above the water level on the steep part of the capillary pressure curve.
FIG. 5 illustrates the log of a clean gas sand in an Indonesian well. A conventional core cut in the bottom half of the sand in oil-base mud shows good porosities, high permeabilities, and low water saturations. The log derived porosities and water saturations were in fairly close correlation with the values obtained by laboratory core analysis. Permeability was calculated from log derived porosity by a correlation designed to maximize agreement with core permeability.
Laboratory measured centrifuge capillary pressure data were available from five cores. Using such data, the coefficients for equations (9) and (10) in the standard model were adjusted to correlate to the measured data from the cores. Equations (9) and (10) adjusted with such data produce local model equations (12) and (13) as follows: ##EQU7##
The coefficient in equation (9) is 5.21 whereas the corresponding coefficient in equation (12) is 3.1. The coefficient in equation (10) is 937.8 whereas the corresponding coefficient in equation (13) is 177. Thus, equations (12) and (13) represent the local model for the Indonesian reservoir.
FIG. 6 also represents the Indonesian well and shows a very close correlation between the water saturations calculated from the equations of the model and the water saturations as measured from the five core samples in the laboratory utilizing the centrifuge. The conversion of capillary pressure Pc to height h is provided by the following equation (14):
h=0.37 Pc (14)
The free-water level was predicted with two different data sets for possible comparison while utilizing the local model for the Indonesian well developed in equations (12) and (13) along with equation (2). For the first set of data, core analysis values for porosity, permeability, and water saturation were entered into the regression at each core plug depth. Based on these values and equations (2), (12), (13), and (14), a free-water level h was predicted 409 feet below the sand base with relatively large error bars. The upper error bar or limit was 56 feet below the sand base.
For the second data set, the porosity, water saturation and air permeability values were derived from a log analysis. Based on these values, a free-water level h was predicted 294 feet below the sand base which was 9,469 feet as illustrated on the log shown in FIG. 5. The error range or error bars were substantially smaller than the error range for the first data set and the upper error range was 134 feet below the sand base. Thus, on the basis of the error range, the free-water level predicted by the log analysis data set is preferred.
A log from a downdip well in the Indonesian reservoir showed a hydrocarbon-water contact 200 feet below the base of the sand as illustrated in FIG. 5. The previous water level predictions from the first data set and the second data set are generally in qualitative agreement with the previous predictions.
When the free-water level is found, this known value may then be utilized to calculate the water saturation at any height in the reservoir. As illustrated in FIG. 5 from the known free-water level as found in the downdip well, water saturation was calculated within the well shown in FIG. 5 and shown on the curve of FIG. 5. The curve indicated a fair to good correlation with the log derived water saturations, except in intervals where the induction resistivity is reduced by thin bed or shoulder bed effects.
FIG. 7 illustrates the log of an oil sand in a well offshore of Ivory Coast, Africa. The resistivity and gamma ray logs show a clean sandstone at the base of the well with a fining upward sequence. Conventional core data at the sand base showed excellent porosity and air permeability. Pressure buildup analysis indicated a kh value of 13,272 md--ft from a drill stem test that flowed 5,000 bo/d. No laboratory measured capillary data were available and prior equations (2), (9) and (10) as set forth below were used for water level prediction. ##EQU8##
For the reservoir fluids present equation (11 ) reproduced again here was used to find the relation h=0.64Pc. ##EQU9##
Log data entered into the regression comprised foot by foot values for porosity, water saturation, and permeability for a 52 foot sandstone interval. Permeability values were calculated from porosity and shaliness using an empirical equation calibrated to the core permeabilities. Based on the above data, the predicted water level h was at 8,500 feet as shown in FIG. 7, or 152 feet below the lowest known oil. The error bars range from 127 feet to 184 feet below the lowest known oil. The water level has not yet been confirmed by a well, but supporting data including a structure map from existing well control and 3-dimensional seismic show a spill point at the predicted water level.
Water saturation was calculated from the predicted free-water level. The water saturations calculated from the predicted free-water level were closely correlated to resistivity based water saturations as shown in FIG. 7. This confirms the method of this invention in relation to the petrophysical data.
Water level predictions according to the present invention have been made in other wells. Listed in Table 2 below are water level predictions from seven different reservoirs or fields. One of the fields, Boomerang, is a limestone reservoir while the other six are sandstone reservoirs.
TABLE 2__________________________________________________________________________FREE-WATER LEVEL PREDICTIONS CONFIRMED BY OTHER DATADistance below lowest known oil Predicted Known Control forField Data free-water level, ft. limits, ft. known limits__________________________________________________________________________Boomerang Crestal well 22 10 Accepted oil/water contactStrawn (oil) Log, conventional coreKent Co., Tex.Stratton Crestal well 6 11 Gas/water contact byD-35 Frio (gas) Log, conventional core, logs and production testsKleberg Co., Tex. capillary pressure dataLake Creek Crestal well 61 51 Lowest known gas fromG-2 Wilcox (gas) Log, conventional core, downdip logMont. Co., Tex. capillary pressure dataUnnamed Discovery well 16 16 Highest known water on log.Miocene (oil) Log, side wall cores, Well cut water after 3 monthsOffshore Louisiana pressure buildupUnnamed Discovery well 11 16 Highest known water on log.Miocene (oil) Log, side wall cores, Well cut water after 6 monthsOffshore Louisiana pressure buildupUnnamed Crestal well 294 200 Gas/water contact fromMiocene (gas) Log, conventional core, downdip logIndonesia capillary pressure dataUnnamed Delineation well 150 150 Structure mapCretaceous (oil) Log, conventional core, spill pointOffshore Africa pressure buildup__________________________________________________________________________
Air permeability ranges from low at Lake Creek field and Stratton field to high in the other four sandstone reservoirs. Three reservoirs, Stratton, Lake Creek, and the unnamed Indonesian reservoir, had capillary pressure Pc data, and equations (9) and (10) were modified to provide a local model for the water level predictions. The remaining four fields utilized the standard model with equations (4), (9), and (10) to predict the free-water level. Fair to good correlations were shown between the free-water level predictions from the standard model and the free-water level predictions calculated from additional data including the capillary pressure Pc data.
The present method of this invention is particularly adapted for use with clastic reservoirs as some of the data utilized in the several equations employed related to sandstone. However, it is believed that the present method may be utilized in other formations, such as carbonates particularly for intercrystalline, intergranular, or interparticle-type textures.
In sandstone reservoirs, porosities have generally exceeded 12 percent. Some applications of the present method have been in low porosity sandstones (4-10%) and satisfactory results have been obtained in the prediction of free-water levels when calibrated with capillary pressure data from specific reservoir rock. For best results in low porosities, capillary pressures should be measured with the cores at reservoir stress. It is noted that when the free-water level is known, the present method can calculate water saturation at any height of the reservoir. These water saturation levels may be compared against resistivity-based water saturations using the standard model. If a relatively close correlation is not obtained, then the model should be adjusted for suitable correlation.
While the method establishing the standard model for this invention has been utilized primarily for the location of free-water levels, if any three of the four basic quantities, porosity, air permeability, water saturation, and capillary pressure are known, then the remaining quantity can be calculated. For example, if the water level is known and the values for porosity and permeability are available, then a water saturation profile can be derived as illustrated by the above case histories of the Indonesian and African wells. The values for water saturations independent of the induction log are particularly useful where sands are thinly laminated with shales.
Another useful application of the method of this invention is the calculation of permeability values when the values for water level, porosity and water saturation are known. In the Lake Creek field set forth in Table 2 above, an effective gas permeability was calculated from the values of water level, porosity, and water saturation. This permeability compared favorably with permeability derived from well tests as indicated in Table 3 below.
TABLE 3______________________________________PERMEABILITY COMPARISONPressure buildup, Capillary pressuremd-ft method, md-ft______________________________________1.3 1.6651.0 9.2812.6 2.5121.0 18.338.0 17.65______________________________________
Equations (1) through (12) listed above are compiled below in Tables 4 and 5 for easy reference together with a definition of the symbols used in the equations.
TABLE 4______________________________________EQUATIONS______________________________________Equation (1) ##STR1##Equation (2) log Pc = -Fg /ln (1 - Sw) + log PdEquation (3) ##STR2##Equation (4) Fg = [ln (1 - Sw)A ]2 /2.303Equation (5) Pd = Pc.sbsb.A (1 - Sw)AEquation (6) log rapex = -0.226 + 0.466 log kaEquation (7) Pc = 107/rapexEquation (8) Pc = 180/ka 0.466Equation (9) ##STR3##Equation (10) Pd = 937.8/(ka 0.3406) φEquation (11) ##STR4##Equation (12) ##STR5##Equation (13) Pd = 177/(ka 0.3406 φ)Equation (14) h = 0.37 Pc______________________________________ where: Fg = Pore geometrical factor, dimensionless rapex = Porethroat radius at Point A, μm h = Height above freewater level, ft. ka = Air permeability, md Pc = Mercury capillary pressure, psi Pd = Mercury displacement pressure, psi Sb = Bulk volume occupied by mercury, % Sb ∞ = Bulk volume occupied by mercury at infinite pressure, % Sw = Water saturation, fraction θr = Contact angle between the water and the reservoir rock (typically 0�) θi = Contract angle between mercury and rock in the laboratory (140�) pw = Formation water density, g/ml ph = Formation hydrocarbon density, g/ml σi = Interfacial tension for mercury in the laboratory, 480 dynes/cm σr = Interfacial tension between the fluids in the reservoir, dynes/cm φ = Porosity, %
As indicated above, equations (2), (9), and (10) were specifically derived for the present invention and may be used when laboratory measured capillary pressure data specific to a reservoir are not available. Water levels are predicted through regression analysis with error ranges being predicted also. In the event laboratory measured capillary pressure data specific to a reservoir are available, the constants in equations (9) and (10) are adjusted as indicated by equations (12) and (13).
While a preferred embodiment of the present invention has been illustrated in detail, it is apparent that modifications and adaptations of the preferred embodiment will occur to those skilled in the art. However, it is to be expressly understood that such modifications and adaptations are within the spirit and scope of the present invention as set forth in the following claims.
|Cited Patent
|Filing date
|Publication date
|Apr 14, 1988
|Feb 20, 1990
|Restech, Inc.
|Method for determining reservoir bulk volume of hydrocarbons from reservoir porosity and distance to oil-water contact level
|AAPG Bulletin Pittman, E.D., Relationship of Porosity and Premeability to Various Parameters Derived from Mercury Injection Capillary Pressure Curves for Sandstone , vol. 76, No. 2, Feb. 1992, pp. 191 198.
|AAPG Bulletin--Pittman, E.D., "Relationship of Porosity and Premeability to Various Parameters Derived from Mercury Injection Capillary Pressure Curves for Sandstone", vol. 76, No. 2, Feb. 1992, pp. 191-198.
|Journal of Petroleum Technology Thomeer, J.H.M., Introduction of a Pore Geometrical Factor Defined by the Capillary Pressure Curve , Mar. 1960 pp. 73 77.
|Journal of Petroleum Technology--Thomeer, J.H.M., "Introduction of a Pore Geometrical Factor Defined by the Capillary Pressure Curve", Mar. 1960 pp. 73-77.
|JPT, Swanson, B.F., "A Simple Correlation Between Permeabilities and Mercury Capillary Pressures", Dec. 1981, pp. 2,498-2,504.
|JPT, Swanson, B.F., A Simple Correlation Between Permeabilities and Mercury Capillary Pressures , Dec. 1981, pp. 2,498 2,504.
|World Oil Smith, D. How to Predict Down Dip Water Level , May 1992, pp. 85 88.
|World Oil--Smith, D. "How to Predict Down-Dip Water Level", May 1992, pp. 85-88.
|Citing Patent
|Filing date
|Publication date
|Nov 13, 1998
|Feb 8, 2000
|Marathon Oil Company
|Determining contact levels of fluids in an oil reservoir using a reservoir contact monitoring tool
|Sep 13, 1999
|Sep 25, 2001
|Electromagnetic Instruments, Inc.
|Electromagnetic induction method and apparatus for the measurement of the electrical resistivity of geologic formations surrounding boreholes cased with a conductive liner
|Aug 24, 2000
|Nov 19, 2002
|Digital Formation Inc.
|System for evaluating fluid distributions of subsurface reservoirs
|Aug 1, 2000
|Apr 1, 2003
|Shell Oil Company
|Method for determining a fluid contact level in a hydrocarbon fluid bearing formation
|Jun 30, 1999
|Sep 9, 2003
|Institut Francais Du Petrole
|Method for gradually deforming a stochastic model of a heterogeneous medium such as an underground zone
|Jan 8, 2004
|Sep 14, 2004
|Schlumberger Technology Corporation
|Method and apparatus for measuring characteristics of geological formations
|Nov 13, 2001
|Sep 14, 2004
|O'meara, Jr. Daniel J.
|Method for determining reservoir fluid volumes, fluid contacts, compartmentalization, and permeability in geological subsurface models
|Jan 23, 2003
|Jun 14, 2005
|Siemens Vdo Automotive Corporation
|System and method for detecting faulty fuel tank level sensor
|Dec 23, 2004
|Apr 18, 2006
|Schlumberger Technology Corporation
|System, apparatus, and method for conducting electromagnetic induction surveys
|Dec 19, 2003
|May 30, 2006
|O'meara Jr Daniel J
|Method for determining reservoir fluid volumes, fluid contacts, compartmentalization, and permeability in geological subsurface models
|May 11, 2006
|Dec 28, 2010
|Schlumberger Technology Corporation
|Simulation method and apparatus for determining subsidence in a reservoir
|Jan 8, 2004
|Jul 29, 2004
|Schlumberger Technology Corporation
|Method and apparatus for measuring characteristics of geological formations
|Dec 23, 2004
|Jul 21, 2005
|Schlumberger Technology Corporation
|System, apparatus, and method for conducting electromagnetic induction surveys
|May 11, 2006
|Nov 20, 2008
|Schlumberger Technology Corporation
|Simulation method and apparatus for determining subsidence in a reservoir
|Mar 21, 2012
|Aug 1, 2012
|Method for determining crack permeability of crack-pore seepage experiment model
|Mar 21, 2012
|May 14, 2014
|Method for determining crack permeability of crack-pore seepage experiment model
|Sep 16, 2011
|Jul 17, 2013
|System and method for estimating fluid distribution in a subterranean reservoir
|Oct 30, 2012
|Jan 29, 2014
|Method for obtaining holding rate of horizontal well through interfacial level
|Oct 30, 2012
|Apr 27, 2016
|Nov 18, 2013
|Mar 26, 2014
|Reservoir classification method and system
|Feb 28, 2014
|May 28, 2014
|Sandstone oil and gas carrier bed geophysics-geology-geochemistry detection method and device
|Apr 4, 2014
|Jun 18, 2014
|Method for distinguishing formation density of carbonatite natural gas reservoir
|Jul 25, 2000
|Feb 8, 2001
|Shell Internationale Research Maatschappij B.V.
|Method for determining a fluid contact level in a formation
|Oct 19, 2012
|Apr 25, 2013
|Saudi Arabian Oil Company
|Methods, computer readable medium, and apparatus for determining well characteristics and pore architecture utilizing conventional well logs
|Oct 19, 2012
|Jun 13, 2013
|Saudi Arabian Oil Company
|Methods, computer readable medium, and apparatus for determining well characteristics and pore architecture utilizing conventional well logs
|U.S. Classification
|73/152.18, 702/13
|International Classification
|Cooperative Classification
|European Classification
|Sep 25, 2000
|Fee payment
Year of fee payment: 4
|Oct 4, 2004
|Fee payment
Year of fee payment: 8
|Jul 31, 2008
|Fee payment
Year of fee payment: 12


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List all words that contain gyred
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Some random words: bulb enate cees groan fyce add wrack
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- Places To Visit
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- Pennsylvania, United States
Northkill Creek is a stream primarily located in Berks County, Pennsylvania. It feeds into Tulpehocken Creek and covers part of the Schuylkill River and Delaware River watersheds. Northkill Creek and its tributaries are high quality trout streams. Northkill Creek begins in the Northkill Gap on Blue Mountain near Shartlesville. The creek flows nearly 11 miles (18 km) roughly south to its Confluence with Tulpehocken Creek just south of Bernville.
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Rivers near Birdsboro
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Baby Name Lists
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Follow along with step-by-step beading projects and share your designs with beaders around the world—it's quick & easy!
- "One the Wings of a Vintaj Butterfly": on
"Ooooooohhhhhhh ... lovely ... aaaaaahhhhhh! What a gorgeous, sweet summer bracelet. Your "borrowed" butterfly…" read »
- "One the Wings of a Vintaj Butterfly": on
"Pam...that's a good question! It's some kind of stone bead..kind of porous looking. I got a…" read »
- "One the Wings of a Vintaj Butterfly": on
"Beautiful bracelet! I love the colors you used. The Vintaj butterflies just add to…" read »
- "Enchanted Forest": on
"Love the rough, chunky feel of this necklace along with the natural wood in this design.…" read »
- "Fun Chunky": on
"'Undesirables'...I have a bin of them too. You did a great job using them--I'd never…" read »
- "Tribal": on
"Those horn beads are just fantastic! Love them with the agate. Definitely a tribal…" read »
- "Gold Glamour": on
"Beautiful necklace--great job highlighting the lampwork focal bead. Love the quartz in this design …" read »
- "Sign of the Cross": on
"What a Stunner! There are so many great things going on in this necklace. …" read »
- "Smaller Staples": on
"Another striking piece made with few materials used in unorthodox ways! Love the bone, copper, and…" read »
- "Thimble of time": on
"Cool! Guess I'll have to shop for a thimble. Haven't had one since 8th grade.…" read »
- "Gold Glamour": on
"Ditto to all of the above comments. A truly magnificent necklace.…" read »
- "Smaller Staples": on
"Thanks everyone. I'm glad you like staples and yes Medieval Momma, this necklace offers protection.…" read »
- "Dysfunctional Limabeader": on
"all of you are very kind with all the wonderful comments! Thank you! I appreciate it!…" read »
- "Dysfunctional Limabeader": on
"These are gorgeous beyond my level to even understand! Wire work is not in my skill…" read »
- "Smaller Staples": on
"This is a great protective necklace, all the eyes to look every way to guard from…" read »
- "Behind the times - Finally made one :)": on
"I haven't made one yet, either. Love the color scheme, love the 2 different sizes of…" read »
- "Thimble of time": on
"Love this! I like the creative use of objects. It is beautiful. Love the colors too…" read »
- "Dysfunctional Limabeader": on
"There's nothing like that gorgeous blue of those agates! And your special wire and beadwork put…" read »
- "Smaller Staples": on
"Very unique and creative. Makes you want to hang onto everything, because you never know…" read »
- "Dysfunctional Limabeader": on
"Beautiful. I love how you embellish the donuts with wirework and beads. It takes…" read »
- "Playing in the Mud x 3 designs": on
"Thanks ladies. I misspelled the product name - it is ceralun clay made by…" read »
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"Very unique!…" read »
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- "Sign of the Cross": on
"This turned out great! I love the colors in this piece, so light and airy, like…" read »
- "Fun Chunky": on
"I envy your ability to use your less desirable beads! I look at mine and groan…" read »
- "Smaller Staples": on
"What a cool idea to use staples! So ingenious! I love this idea and design!…" read »
- "Playing in the Mud x 3 designs": on
"If this clay is as easy to use as it is beautiful, I definitely need to…" read »
- "Enchanted Forest": on
"This is super cute!…" read »
- "Fun Chunky": on
"Ditto to all of the above. This turned out awesome!…" read »
- "Smaller Staples": on
"The staples with the bone are very beautiful!…" read »
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"Knew this was yours as soon as I saw it! Love the staples with the bone.…" read »
- "Behind the times - Finally made one :)": on
"LOVE the color combo and the bracelet!! I had never thought of making one, but.....…" read »
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About this design:
More scary earring pics! So hard to get a good photo! Anyway, more ocean inspired earware.
The Czech glass is either Peruvian Opal or Beach Glass...either way, there's alot more yellow going on than meets the eye. Didn't realize it until last night's Art Walk...but it's all good!
Components:Patina'd brass blanks, Czech glass, and brass earwires.
Read the comments (or add your own)
Just love your patina work! The pop of green in the corner of the czech glass, really pop out that color in your patina work. Another gorgeous pair of earrings Susie!
Love these, too!! I haven't made earrings or patina'ed anything in awhile but these have just given me a kick in the butt and some ideas!
Art Walk? Do tell!
Very pretty. How do you apply the patina? drop a bit and let it roll around?
And buff the areas that you want highlighted?
Thanks Wanda and Becky!
Art Walk….Let's see…Gulfport is often considered to be an Artist Colony. There are many resident artists, and the Industrial Arts Center, plus lots of galleries along Beach Boulevarde.
Gulfport has a First Friday and 3rd Saturday Art Walk every month that features local artisans at an evening festival from 6-10PM. As of late, some of it is pretty trashy, so the city is attempting to revamp it all, with the 1st Friday being Fine Arts Friday…that is my goal for next month. And Geckofest….an Arts and Crafts festival to celebrate the end of summer..10A to 10P, with 30K expected attendess. I'd love to have some visitors for that one!(hint hint).
Anyway, the green in the Czech glass squares was really yellow under the halogen lights at the Art Walk last night. The booth looked beautiful in all that light, but I forgot to take a picture!
Hi Peggy! I use a paper plate to combine my patina colors. I like a pea sized drop of color to a nickle sized drop of patina glaze and extender. Then I use a wet brush to apply a base color, and dab the other colors to the blank. I tilt the blank in different directions to achieve the tie dye affect.
I love the colors you used. Simply stunning.
An art walk sounds like loads of fun, I wish they had something like that around here!
Love them…I love the embossing so much. Want a Big Kick!!! As usual your patina is fantastic.
Pretty and dramatic. Wearing these would bring lots of compliments.
I admire what you do with metals…so pretty.
I am loving all your patina piece…this is so lovely! We used to have so many arts/crafts things around here, and its dwindled down to a few. I wish we still had them all.
Ooops….make that PIECES! Its been a long day! LOL
What cool earrings!
You are doing a great job with this technique. It is one of my favorites, too.
You have clearly perfected your patina technique, Susie ! These are yet another pair of stunning earrings – - -
The art walk sounds like a blast and you're certainly doing your part in bringing the standards up! Love these!
Love these earrings!
Beautiful earrings!
I'm lovin these,E.M!
These are so much fun.
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Zach Galifianakis's photobomb among top TODAY GIFsPlay Video
More video
Ticketmaster vouchers: Why some customers aren't happy with free tickets
Dino-sorehead: Teen gets her head stuck in Barney costume
Rare 'strawberry moon' has social media seeing red
What are your pets up to when you leave the house?
GIFs are good for many things but maybe their best use is re-living the most hilarious, adorable, awkward and otherwise incredible moments on TODAY in 2013, over and over and over again.
They are, of course, presented in no particular order. Scroll down and vote on which of the chosen GIFs are your favorite!
1. Zach Galifianakis photobombs Natalie during the news.
2. Paula Patton dances for Al.
3. Matt Lauer as Pamela Anderson. Enough said.
4. David Gregory does Gangnam style.
5. Tamron Hall attacked by puppies.
6. Al and Willie canoodling in a canoe.
7. Kathie Lee and Hoda locking (wax) lips.
8. Al and Willie kiss on camera (seeing a theme here?)
9. Savannah gets pie to the face and falls with Jimmy Fallon.
10.Carson Daly taking out Natalie's Barbie dolls with his X-wing.
11. Natalie as a fox.
12. Most shocked Ambush Makeover contestant ever?
13. Bill Cosby getting ready for his interview.


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Return to SwingLifeStyle.com The Swingers Home Page
There are a total of 16660 Averill Park swingers, within 100 miles.
The list below is a subset of the swingers in the Averill Park area.
Create a free swingers account so you can see and write to them all.
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Fun sized and adventurous
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Sexy couple looking to please and be pleased!
Sexy Couple Looking to experiment
Older experienced swinger, looking for threesomes or moresomes who LUV getting NASTY!
Lets make some "Hot Summer nights!"
Enjoy having fun.... Join Me !!
Looking to meet a new couple.
First timers
Looking around
Just looking for some clean (sometimes kinky) adult fun!
Live Laugh Love
lets get together see where it goes !! have a party coming up !
Here to make fun friends
Looking for FWB! Can Host & Travel
MW Attractive easy going
Special thanks to all our new friends - had a great time at the New Year's Eve party
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Accordingly, neither this site nor the contents contained herein are covered by the record-keeping provisions of 18 USC 2257(a)-(c).
Disclaimer: This website contains adult material. You must be over 18 to enter or 21 were applicable by law.
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Mission to Mars
After 250 days in a locked, windowless steel capsule, researchers on a mock trip to Mars ventured from their cramped quarters in heavy space suits, trudging into a sand-covered room to plant flags on a simulated Red Planet.
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Canon has announced that since its 2004 introduction of the DIGISUPER 22xs lens (model XJ22x7.3B IE-D), TV production companies and broadcasters have purchased the lenses as part of their transition to HDTV.
Canon's compact studio HD lens provides "box lens" optical performance in a compact size scaled to portable HD cameras.
The DIGISUPER 22xs Compact Studio HD Lens is a high-end optical system based upon Canon's classic studio lens design principles but carefully constrained to a physical size and weight (13.4lbs) commensurate with that of contemporary portable production cameras.
The lens offers Canon's exclusive eDrive system. Together with its optical encoders, eDrive provides lens-status information on an easy-to-read display that accurately reports settings for f-stop, focal length, focusing distance and other parameters.
For more information, visit: www.usa.canon.com.
Scaled-Up Starz a Winner in Lionsgate Marriage
West Virginia TV Bands Together for Flood Victims
NAB FOIA's FCC Media Ownership Work Product
HTC Leads $10B Virtual Reality VC
NCTA: Sloganeering Doesn't Make Set-Top Plan Lawful
Comcast Backs Off Planned Upgrade of Legacy Set-Top Guide
NASA arrives on Apple TV
AMC partner with Machinima for SVoD gaming channel
NRK invests in Tedial Evolution
Rob Burnett Makes a Laugh-Out-Loud Dramedy with 'The Fundamentals of Caring'
New Lifetime Docuseries Focuses on Families of Olympic Hopefuls
FAA's New Drone Rule Gets Mixed Responses


text:
Miller will request a recount in Waukesha's District 11 aldermanic election
Eight votes separated challenger, incumbent
Eight votes were all that separated Roger Patton, the incumbent, and his challenger Lenny Miller in Tuesday's District 11 aldermanic election.
Given the razor-thin margin, 202 votes to 194, Miller said Friday that he will request a recount.
"With it being so close, I just want to rule out any errors or voter machine malfunctions," Miller said. "Every vote counts."
The votes must be canvassed, which will be done on Monday, City of Waukesha Deputy Clerk-Treasurer Gina Kozlik said.
Miller will then send a recount petition to the clerk's office.
The recount will cost Miller $25 at $5 per ward.
Kozlik said the city was still counting late absentee ballots as of Friday but only one came from that district.
"There were no problems on election day and I don't anticipate a change," Kozlik said. "But we certainly expected a recount when it was that close."
If the vote stands, it will mark the second straight win for Patton over Miller. Patton, a retired minister, defeated Miller in 2010.
However, of all the races in Waukesha that were challenged this year, District 11 was the closest by far.
"I was surprised (by the outcome)," Miller said. "Before the election, I was knocking on doors for two weeks and the message I was getting was that they'd vote for me. They were glad someone else was running. So I'm surprised and disappointed."
There was a 16.6 voter turnout in District 11, the fourth lowest in the city.
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Father's Day Crafts
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Bashore Family History & Genealogy
Find Bashore recordsSearch for Bashore records
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Bashore Bios
Find records of Bashores by their first name:
- Ada Bashore to Betty Bashore
- Beverly Bashore to Clem Bashore
- Clifford Bashore to Duane Bashore
- Earl Bashore to Frances Bashore
- Francis Bashore to Herbert Bashore
- Herman Bashore to Joe Bashore
- John Bashore to Lillie Bashore
- Lily Bashore to Mary Bashore
- Mason Bashore to Neill Bashore
- Nellie Bashore to Robert Bashore
- Roger Bashore to Terrence Bashore
- Terri Bashore to Zora Bashore
Most Common First Names
- John 3.1%
- Harold 1.7%
- William 1.7%
- George 1.7%
- Robert 1.6%
- David 1.6%
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- Dorothy 1.2%
- Richard 1.2%
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These are the longest-lived members of the Bashore family on AncientFaces.
- Anna J Bashore lived 104 years
- Iva B Bashore lived 102 years
- Emma M Bashore lived 101 years
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Ngoc Yen Hotel
Address153 Mac Thien Tich, Binh San Ward Ha TienSee nearby area
For rates, enter dates/guests
Description provided by property
Ngoc Yen Hotel is located in Ha Tien, 22 km from Kep.
Every room has a TV. All rooms are fitted with a private bathroom. Ngoc Yen Hotel features free WiFi throughout the property.
You will find a 24-hour front desk at the property.
The nearest airport is Phu Quoc International Airport, 59 km from Ngoc Yen Hotel.
Services & facilities
- Family rooms
Guest services
- 24-hour front desk
Wi-Fi/internet access
- Free WiFi
Nearby places
Dong Ho
The name translates as East Lake, but Dong Ho is not a lake but an inlet of the sea. Dong Ho is said to be most beautiful on nights when...
Pirate Island
This small speck of an island, its hill covered in lush vegetation, has a sordid 500-year history as a pirate haven, which only came to...
Thach Dong Cave Pagoda
Also known as Chua Thanh Van, this Buddhist cave temple is 4km northeast of town. Scramble through the cave chambers to see the funerary...
Floating Restaurant
Smartly refurbished and sitting by the River Hotel, this cheery boat is a good bet on weekends, when a team of chefs is on hand to feed...


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A highly banned and controversial substance in the Cosmic Era
One of the strangest weapons deployed by Z'pl'rt the Mad
Admirals, I present to you the future of space warfare! No longer will you need to waste billions of credits on costly space battles, and millions of lives on planetary warfare with hostile cultures. For only a fraction of the cost of a heavy cruiser, I present you with a weapon capable of eliminating an entire solar system. "I present the Star Hammer!"
(A powerful and deviously simple weapon to make space warfare in any sci-fi game forever changed)
I once read a book about a group of people who discovered a hidden temple city in a mountain range, where the Incas-the ancient civilisation of Peru- had fled to when the spanish invaded. When this group found the burial chamber of one of the inca high priests, they unleashed a powerful curse upon them all...


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Potato Salad in Radicchio Cups
From EatingWell: November/December 2007
With a store-bought or leftover roasted chicken, this hearty curried chicken salad is ready in a snap.
Makes: 2 dozen appetizers
Active Time:
Total Time:
Nutrition Profile
Diabetes appropriate | Low carbohydrate | Gluten free |View Our Nutrition Guidelines »
- 8 ounces Yukon Gold potatoes, peeled and cut into 1/4-inch pieces (about 1 1/3 cups)
- 5 tablespoons reduced-fat mayonnaise
- 1 tablespoon lemon juice
- 1 teaspoon curry powder
- 1/2 teaspoon salt
- 1/4 teaspoon freshly ground pepper
- 1 cup chopped skinless roasted chicken
- 1/3 cup diced peeled tart green apple
- 3 tablespoons diced red onion
- 3 tablespoons diced red bell pepper
- 3 tablespoons diced celery
- 2 tablespoons chopped golden raisins
- 24 small radicchio, Boston lettuce or endive leaves
- Bring a small saucepan of water to a boil. Add potatoes; cook until just tender, 7 to 9 minutes. Drain and let cool for 10 minutes.
- Whisk mayonnaise, lemon juice, curry powder, salt and pepper in a medium bowl until smooth. Stir in chicken, apple, onion, bell pepper, celery, raisins and the cooled potatoes.
- Place about 2 tablespoons potato salad in each radicchio (or lettuce or endive) leaf.
Tips & Notes
- Make Ahead Tip: Prepare through Step 2, cover and refrigerate for up to 2 days.
Per appetizer: 30 calories; 1 g fat (0 g sat, 0 g mono); 5 mg cholesterol; 4 g carbohydrates; 0 g added sugars; 2 g protein; 0 g fiber; 84 mg sodium; 63 mg potassium.
Carbohydrate Servings: 1/2
Exchanges: 1/2 starch, 1/2 fat (for 2 appetizers)
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Recipe Categories
- Ease of Preparation
- Moderate
- Total Time
- 45 minutes or less
- Style/Theme
- Comfort foods
- Make ahead instructions
- Picnic
- Potluck
- Servings
- 8 or more
- Main Ingredient
- Chicken
- Meal/Course
- Appetizers
- Type of Dish
- Appetizer
- Ethnic/Regional
- American
- Health & Diet Considerations
- Diabetes appropriate
- Low carbohydrate
- Gluten free
- Publication
- November/December 2007