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Should I Pay $71 To see My OurTime Flirts?

May 12, 2011 Filed Under: Dating Markets

[Editor note: This post is the most popular one on this blog and has been for a long time. Who knew?]

After signing up yesterday with a silly profile and ugly photo, I’ve received my first flirt from the new Match over-50 dating site, OurTime .

This is where I really feel for singles. Do I pay $20, $53 or $71 to see who flirted with me? In any other context, paying $20 to read an email is insane. Especially when it’s only a wink. Dating sites really have no option but to work this way. Its unfortunate but how else are they going to get free members to convert to subscribers?

If I knew the flirt was from a verified member, I probably would be more likely to pay up, but the fact that they don’t show the person’s photo or username or a bit of text from/about them has me on the defensive.

I’m talking to OurTime tomorrow, should be able to report back with some clarity on where the profiles are being copied over from and other details about the launch.

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Dating

Dating is a part of human mating process whereby two people meet socially for companionship. beyond the level of friendship. or with the aim of each assessing the other's suitability as a partner in an intimate relationship or marriage. It can be a form of courtship consisting of social activities done by the couple. While the term has several meanings, it usually refers to the act of meeting and engaging in some mutually agreed upon social activity in public, together, as a couple.

History [ edit ]

Dating as an institution is a relatively recent phenomenon which has mainly emerged in the last few centuries. From the standpoint of anthropology and sociology. dating is linked with other institutions such as marriage and the family which have also been changing rapidly and which have been subject to many forces, including advances in technology and medicine. As humans have evolved from hunter-gatherers into civilized societies and more recently into modern societies, there have been substantial changes in the relationship between men and women, with perhaps the only biological constant being that both adult women and men must have sexual intercourse for human procreation to happen. [ 3 ]

Humans have been compared to other species in terms of sexual behavior. Neurobiologist Robert Sapolsky constructed a reproductive spectrum with opposite poles being tournament species. in which males compete fiercely for reproductive privileges with females, and pair bond arrangements, in which a male and female will bond for life. [ 4 ] According to Sapolsky, humans are somewhat in the middle of this spectrum, in the sense that humans form pair bonds, but there is the possibility of cheating or changing partners. [ 4 ] These species-particular behavior patterns provide a context for aspects of human reproduction. including dating. However, one particularity of the human species is that pair bonds are often formed without necessarily having the intention of reproduction. In modern times, emphasis on the institution of marriage, generally described as a male-female bond, has obscured pair bonds formed by same-sex and transsexual couples, and that many heterosexual couples also bond for life without offspring, or that often pairs that do have offspring separate. Thus, the concept of marriage is changing widely in many countries.

Historically, marriages in most societies were arranged by parents and older relatives with the goal not being love but legacy and "economic stability and political alliances", according to anthropologists. [ 5 ] Accordingly, there was little need for a temporary trial period such as dating before a permanent community-recognized union was formed between a man and a woman. While pair-bonds of varying forms were recognized by most societies as acceptable social arrangements, marriage was reserved for heterosexual pairings and had a transactional nature, where wives were in many cases a form of property being exchanged between father and husband, and who would have to serve the function of reproduction. Communities exerted pressure on people to form pair-bonds in places such as Europe ; in China. according to sociologist Tang Can, society "demanded people get married before having a sexual relationship" [ 6 ] and many societies found that some formally recognized bond between a man and a woman was the best way of rearing and educating children as well as helping to avoid conflicts and misunderstandings regarding competition for mates.

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Search Telegraph Dating

Posted in the Human Sexuality Forum

#12 Dec 25, 2012

I screwed a 68 year old woman she really like to do it during the day when we would meet and talk that's all she could tell me about so one night when I was over to her house this was the first time we were gonna have sex I was sold excited there was nobody around to stop me she wanted me to give her a kiss I gave read the passionate kiss and to my arms around her and whispered in her ear

The Fame

Released: April 8, 2008 ( 2008-04-08 )

"Poker Face "

Released: September 23, 2008 ( 2008-09-23 )

"Eh, Eh (Nothing Else I Can Say) "

Released: January 10, 2009 ( 2009-01-10 )

"LoveGame "

Released: March 24, 2009 ( 2009-03-24 )

"Paparazzi "

Released: July 6, 2009 ( 2009-07-06 )

The Fame is the debut studio album by American recording artist Lady Gaga. It was released on August 19, 2008 through Interscope Records. After joining Kon Live Distribution and Cherrytree Records in 2008, Gaga began working on the album with different producers, primarily RedOne. Martin Kierszenbaum and Rob Fusari. Musically, The Fame is a synthpop and dance-pop album that has influences of pop music from the 1980s. Lyrically, the album visualizes Gaga's love of fame in general while also dealing with subjects such as love, sex, money, drugs and sexual identity. Promotion was primarily through The Fame Ball Tour and multiple television appearances. The Fame was included as a bonus disc on the deluxe edition of the extended play, The Fame Monster (2009).

The album received generally favorable reviews from music critics, who commended the album's lyrical content and Gaga's musicianship and vocal ability, which have been compared to fellow pop singers such as Gwen Stefani. The album was a commercial success, topping the charts in different countries worldwide, including the United Kingdom, Canada, Germany, Ireland, Poland and Switzerland. In the United States, it peaked at number two on the Billboard 200. while topping the Dance/Electronic Albums chart for 106 non-consecutive weeks.

The first two singles from The Fame . "Just Dance " and "Poker Face ", gained international success, topping the charts in several countries worldwide, including the United States, United Kingdom and Australia. "LoveGame " and "Paparazzi ", were commercial successes as well, charting within the top ten of more than ten countries worldwide. "Eh, Eh (Nothing Else I Can Say) " had a limited release in some countries, while "Beautiful, Dirty, Rich " was released in the form of a promotional single.

Contents

Background and development [ edit ]

While establishing herself as an artist and working her way up through the New York underground club scene, Gaga released her debut studio album, The Fame . [ 5 ] Speaking about the title and concept of the album, Gaga explained: " The Fame is about how anyone can feel famous. [. ] Pop culture is art. It doesn't make you cool to hate pop culture, so I embraced it and you hear it all over The Fame . But, it's a sharable fame. I want to invite you all to the party. I want people to feel a part of this lifestyle." [ 6 ] Gaga stated in an interview with MTV UK that she had been working on the album for two and a half years and completed half of it during the first week of January 2008. [ 7 ] As well as writing the lyrics, Gaga worked on the melodies and synth work of the album, with record producer RedOne. [ 6 ] According to Gaga, the first track "Just Dance " is a joyous, heart-themed song, which appeal to people going through tough times in their life. [ 8 ] "LoveGame ", the second track, was inspired by Gaga's sexual crush on a stranger in a night club to whom she said, "I wanna ride on your disco stick". It was written in four minutes based on the disco stick hook. [ 9 ] "Paparazzi " has been interpreted with different meanings. However Gaga explained in an interview with About. com. that the song was inspired by her struggles and hunger for fame and love. Essentially a love song, "Paparazzi" dealt with enticing the media and asked the question, whether one can have both fame and love. [ 10 ]

"Poker Face " was inspired by Gaga's boyfriends who enjoyed gambling, and also dealt with her personal experience of bisexuality ; her fantasies about women while having sex with men, thus representing her 'poker face'." [ 11 ] [ 12 ] "Boys, Boys, Boys" was inspired by the similarly titled Motley Crue song "Girls, Girls, Girls ". Gaga explained that she wanted a female version of the song that rockers would like too. [ 6 ] "Beautiful, Dirty, Rich " summed up her time of self-discovery, living in the Lower East Side and dabbling in drugs and the party scene. [ 6 ] "Eh, Eh (Nothing Else I Can Say) " was about breaking up with a boyfriend and finding someone new. [ 6 ] "Brown Eyes" was inspired by the British rock band Queen and, according to Gaga, is the most vulnerable song on the album. [ 6 ]

Gaga further clarified the ideas behind The Fame . and her inspirations and visions for the album. She believed that the most important thing missing from contemporary pop music was the combination of the visual imagery of the artist with the music. Gaga incorporated theatrics in her live performances of the songs from the album. Hence she hoped that people would take notice of the performance art. which she was trying to bring back with the album and its music; according to her, the music put the lifestyle in front of it. [ 13 ]

"I just feel like this record is really different - you[']ve got club bangers to more 70s glam to more singer-songwriter records to rock music. [. ] The Fame is not about who you are—it's about how everybody wants to know who you are! Buy it and listen to it before you go out or in the car. [. ] I think you've really got to allow artists' creativity to marinate. It took me a while but really delving into myself I finally got it. I couldn't be more proud of it. It's not just a record[,] it's a whole pop art movement[.] It's not just about one song." [ 7 ]

Composition [ edit ]

Musically, the album drew influences from late 1970s glam rock musicians such as David Bowie and Queen. Gaga incorporated their glam-rock sound while devising catchy pop melodies and hooks to create what she has dubbed, "theatrical pop". [ 14 ] Songs like "Poker Face ", "Just Dance " and "LoveGame " are uptempo dance songs, with "Poker Face" carrying a dark sound with clear vocals on the chorus and a pop hook. [ 15 ] "Just Dance" is synth-based while "LoveGame" has a more dance-oriented beat, and "Money Honey" has a moderate techno groove. [ 16 ] All of them combined synths of clipped marching beats, sawing electronics and contained mild R&B - infused beats. [ 17 ] "Paparazzi" carried a sultry beat [ 18 ] while "Summerboy" had influences of the music of Blondie. [ 14 ] "Eh, Eh (Nothing Else I Can Say) " is credited as a ballad compared to the rest of the dance-fueled tracks from The Fame . [ 2 ] The song has a 1980s synthpop feeling in it, [ 18 ] while incorporating the "Eh, Eh" hook from Rihanna 's single "Umbrella " (2007). [ 19 ]

"This idea of The Fame runs through and through. Basically, if you have nothing—no money, no fame—you can still feel beautiful and dirty rich. It's about making choices, and having references—things you pull from your life that you believe in. It's about self-discovery and being creative. The record is slightly focused, but it's also eclectic.[. ] The music is intended to inspire people to feel a certain way about themselves, so they'll be able to encompass, in their own lives, a sense of inner fame that they can project to the world, and the carefree nature of the album is a reflection of that aura. I like to funnel interesting ideas to the rest of the world through a pop lens." [ 13 ]

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Thursday, 27 February 2014

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С какими брокерами я зарабатываю на Форекс?

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Dating

History [ edit ]

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Thank you! I've found my man! Great!

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History [ edit ]

How To Come Together In Perfect 69 Harmony

The novelty of being pleasured while pleasuring her is well worth the effort.

Page 1 of 2

Some people like to give and some like to receive, but with the 69 position you can have the best of both worlds. This position is designed for mutual, simultaneous oral sex. It may be a little difficult to concentrate on what you’re doing with your tongue when she’s busy at work between your legs, but the novelty of being pleasured while pleasuring her is well worth the effort.

When it comes to 69ing, there are some dos and don’ts in order to make it a pleasurable experience for both of you. For the purposes of this article, we’re referring to 69ing as foreplay. so we won’t cover ejaculation etiquette. which inspired an entire article of its own.

Take A Shower

As with all sexual acts, especially those involving oral stimulation, it’s imperative to be clean and well groomed down below. Nobody wants to be greeted by unpleasant odors or a jungle of hair; this is bad 69 etiquette. So if you’re going to try out the 69 position, clean up and keep it trimmed. Better yet, jump in the shower together so you can ensure both of you smell and taste fresh and clean.

Initiate Gradually

You should make a point of easing her into it, especially if it’s the first time you’ve 69ed with her. Don’t just throw her on top. Make the transition part of your foreplay and gradually get into position. She should take the hint from there.

She Goes On Top

If one of you has to be on top in the 69 position, it should always be the girl. Chances are, you are heavier than she is, and allowing her to take the top position will prevent her from being crushed if the 69 session takes a while or if you get too carried away. This also helps you to avoid accidentally kneeling on her hair. Another benefit of her being on top is that she can control the speed, depth and angle of penetration, so you’re less likely to accidentally gag her. Letting her have control means better oral pleasure for you, so this is really a no-brainer in terms of 69 etiquette.

The 69 position can also be done with both of you laying on your sides, which may be a more comfortable option if you plan to keep it going for a longer period of time. This way, you can use each other’s inner thighs as pillows for your heads, making the arrangement very comfy for a more drawn out 69 session.

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Radiocarbon dating

From Wikipedia, the free encyclopedia

Radiocarbon dating is a method of determining the age of an object by using the properties of radiocarbon. a radioactive isotope of carbon. The method was invented by Willard Libby in the late 1940s and soon became a standard tool for archaeologists. It depends on the fact that radiocarbon, often abbreviated as 14

C. is constantly being created in the atmosphere by the interaction of cosmic rays with atmospheric nitrogen. The resulting radiocarbon combines with atmospheric oxygen to form radioactive carbon dioxide. This is then incorporated into plants by photosynthesis. and animals acquire 14

C by eating the plants. When the animal or plant dies, it stops exchanging carbon with its environment, and from that point the amount of 14

C it contains begins to reduce as the 14

C undergoes radioactive decay. Measuring the amount of 14

C in a sample from a dead plant or animal such as piece of old wood or a fragment of bone provides information that can be used to calculate when the animal or plant died. The oldest dates that can be reliably measured by radiocarbon dating are around 50,000 years ago, though special preparation methods occasionally permit dating of older samples.

While the idea behind radiocarbon dating is straightforward, years of additional work were required to develop the technique to the point where accurate dates could be obtained. Research has been going on since the 1960s to determine what the proportion of 14

C in the atmosphere has been over the past fifty thousand years. The resulting data, in the form of a calibration curve, is now used to convert a given measurement of radiocarbon in a sample into an estimate of the sample's actual calendar age. In addition to this curve, other corrections must be made to account for different proportions of 14

C in different types of organism (fractionation) and different 14

C levels in different parts of the biosphere (reservoir effects).

Measurement of radiocarbon was originally done by beta-counting devices, so called because they counted the amount of beta radiation emitted by decaying 14

C atoms in a sample. More recently, accelerator mass spectrometry has become the method of choice; it can be used with much smaller samples (as small as individual plant seeds), and gives results much more quickly.

The development of radiocarbon dating has had a profound impact on archaeology. In addition to permitting more accurate dating within archaeological sites than did methods previously in use, it also allows comparison of dates of events across great distances. Histories of archaeology often refer to the early impact of the new method as the “radiocarbon revolution”. Occasionally, the method is used for items of popular interest such as the Shroud of Turin. which is claimed to show an image of the body of Jesus Christ. A sample of linen from the shroud was tested in 1988 and found to date from the 1200s or 1300s, casting doubt on its authenticity.

Contents

Background [ edit ]

History [ edit ]

In the early 1930s Willard Libby was a chemistry student at the University of Berkeley. receiving his Ph. D. in 1933. He remained there as an instructor until the end of the decade. In 1939 the Radiation Laboratory at Berkeley began experiments to determine if any of the elements common in organic matter had isotopes with half-lives long enough to be of value in biomedical research. It was soon discovered that 14

C 's half-life was far longer than had been previously thought, and in 1940 this was followed by proof that the interaction of slow neutrons with 14

N was the main pathway by which 14

C was created. It had previously been thought 14

C would be more likely to be created by deuterons interacting with 13

C. At about this time Libby read a paper by W. E. Danforth and S. A. Korff, published in 1939, which predicted the creation of 14

C in the atmosphere by neutrons from cosmic rays which had been slowed down by collisions with molecules of atmospheric gas. It was this paper that first gave Libby the idea that radiocarbon dating might be possible. [ 1 ]

In 1945, Libby moved to the University of Chicago. He published a paper in 1946 in which he proposed that the carbon in living matter might include 14

C as well as non-radioactive carbon. [ 2 ] [ 3 ] Libby and several collaborators proceeded to experiment with methane collected from sewage works in Baltimore, and after isotopically enriching their samples they were able to demonstrate that they contained radioactive 14

C. By contrast, methane created from petroleum had no radiocarbon activity. The results were summarized in a paper in Science in 1947, and the authors commented that their results implied it would be possible to date materials containing carbon of organic origin. [ 2 ] [ 4 ]

Libby and James Arnold proceeded to experiment with samples of wood of known age. For example, two wood samples taken from the tombs of two Egyptian kings, Zoser and Sneferu. independently dated to 2625 BC plus or minus 75 years, were dated by radiocarbon measurement to an average of 2800 BC plus or minus 250 years. These results were published in Science in 1949. [ 5 ] [ 6 ] In 1960, Libby was awarded the Nobel Prize in Chemistry for this work. [ 2 ]

Physical and chemical details [ edit ]

In nature, carbon exists as two stable, nonradioactive isotopes. carbon-12 ( 12

C ), and a radioactive isotope, carbon-14 ( 14

C ), also known as "radiocarbon". The half-life of 14

C (the time it takes for half of a given amount of 14

C to decay ) is about 5,730 years, so its concentration in the atmosphere might be expected to reduce over thousands of years. However, 14

C is constantly being produced in the lower stratosphere and upper troposphere by cosmic rays. which generate neutrons that in turn create 14

C when they strike nitrogen-14 ( 14

N ) atoms. [ 2 ] The 14

C creation process is described by the following nuclear reaction :

Once produced, the 14

C quickly combines with the oxygen in the atmosphere to form carbon dioxide ( CO

2 ). Carbon dioxide produced in this way diffuses in the atmosphere, is dissolved in the ocean, and is taken up by plants via photosynthesis. Animals eat the plants, and ultimately the radiocarbon is distributed throughout the biosphere. The ratio of 14

Principles [ edit ]

During its life, a plant or animal is exchanging carbon with its surroundings, so the carbon it contains will have the same proportion of 14

C as the biosphere and the carbon exchange reservoir. Once it dies, it ceases to acquire 14

C. but the 14

C within its biological material at that time will continue to decay, and so the ratio of 14

C to 12

C in its remains will gradually reduce. Because 14

C decays at a known rate, the proportion of radiocarbon can be used to determine how long it has been since a given sample stopped exchanging carbon—the older the sample, the less 14

C will be left. [ 8 ]

The equation governing the decay of a radioactive isotope is: [ 2 ]

where N 0 is the number of atoms of the isotope in the original sample (at time t = 0, when the organism from which the sample was taken died), and N is the number of atoms left after time t . [ 2 ] ? is a constant that depends on the particular isotope; for a given isotope it is equal to the reciprocal of the mean-life — i. e. the average or expected time a given atom will survive before undergoing radioactive decay. [ 2 ] The mean-life, denoted by ? . of 14

C is 8,267 years, so the equation above can be rewritten as: [ 11 ]

The sample is assumed to have originally had the same 14

C / 12

C ratio as the ratio in the biosphere, and since the size of the sample is known, the total number of atoms in the sample can be calculated, yielding N 0 . the number of 14

C atoms in the original sample. Measurement of N . the number of 14

C atoms currently in the sample, allows the calculation of t . the age of the sample, using the equation above. [ 8 ]

The half-life of a radioactive isotope (the time it takes for half of the sample to decay, usually denoted by t 1/2 ) is a more familiar concept than the mean-life, so although the equations above are expressed in terms of the mean-life, it is more usual to quote the value of 14

C 's half-life than its mean-life. [ note 1 ] The currently accepted value for the half-life of 14

C is 5,730 years. [ 2 ] This means that after 5,730 years, only half of the initial 14

C will have remained; a quarter will have remained after 11,460 years; an eighth after 17,190 years; and so on.

The above calculations make several assumptions, such as that the level of 14

C in the biosphere has remained constant over time. [ 2 ] In fact, the level of 14

C in the biosphere has varied significantly and as a result the values provided by the equation above have to be corrected by using data from other sources in the form of a calibration curve, which is described in more detail below. [ 12 ] For over a decade after Libby's initial work, the accepted value of the half-life for 14

C was 5,568 years; this was improved in the early 1960s to 5,730 years, which meant that many calculated dates in published papers were now incorrect (the error is about 3%). However, it is possible to incorporate a correction for the half-life value into the calibration curve, and so it has become standard practice to quote measured radiocarbon dates in "radiocarbon years", meaning that the dates are calculated using Libby's half-life value and have not been calibrated. [ 13 ] [ note 2 ] This approach has the advantage of maintaining consistency with the early papers, and also avoids the risk of a double correction for the Libby half-life value. [ 15 ]

Carbon exchange reservoir [ edit ]

Simplified version of the carbon exchange reservoir, showing proportions of carbon and relative activity of the 14

The different elements of the carbon exchange reservoir vary in how much carbon they store, and in how long it takes for the 14

C generated by cosmic rays to fully mix with them. [ 2 ] The atmosphere, which is where 14

C is generated, contains about 1.9% of the total carbon in the reservoirs, and the 14

C it contains mixes in less than seven years. [ 16 ] [ 17 ] The ratio of 14

C to 12

C in the atmosphere is taken as the baseline for the other reservoirs: if another reservoir has a lower ratio of 14

C to 12

C. it indicates that the carbon is older and hence that some of the 14

C has decayed. [ 12 ] The ocean surface is an example: it contains 2.4% of the carbon in the exchange reservoir, [ 16 ] but there is only about 95% as much 14

C as would be expected if the ratio were the same as in the atmosphere. [ 2 ] The time it takes for carbon from the atmosphere to mix with the surface ocean is only a few years, [ 18 ] but the surface waters also receive water from the deep ocean, which has over 90% of the carbon in the reservoir. [ 12 ] Water in the deep ocean takes about 1,000 years to circulate back through surface waters, and so the surface waters contain a combination of older water, with depleted 14

C. and water recently at the surface, with 14

C in equilibrium with the atmosphere. [ 12 ]

Creatures living at the ocean surface have the same 14

C ratios as the water they live in, and as a result of the reduced 14

C / 12

C ratio, the radiocarbon age of marine life is typically about 400 years. [ 19 ] [ note 4 ] Organisms on land, however, are in closer equilibrium with the atmosphere and have the same 14

C / 12

C ratio as the atmosphere. [ 2 ] These organisms contain about 1.3% of the carbon in the reservoir; sea organisms have a mass of less than 1% of those on land and are not shown on the diagram. [ 16 ] Accumulated dead organic matter, of both plants and animals, exceeds the mass of the biosphere by a factor of nearly 3, and since this matter is no longer exchanging carbon with its environment, it has a 14

C / 12

Dating considerations [ edit ]

The variation in the 14

C / 12

C ratio in different parts of the carbon exchange reservoir means that a straightforward calculation of the age of a sample based on the amount of 14

C it contains will often give an incorrect result. There are several other possible sources of error that need to be considered. The errors are of four general types:

variations in the 14

C / 12

C ratio in the atmosphere, both geographically and over time;

isotopic fractionation;

variations in the 14

C / 12

C ratio in different parts of the reservoir;

contamination.

Atmospheric variation [ edit ]

In the early years of using the technique, it was understood that it depended on the atmospheric 14

C / 12

C ratio having remained the same over the preceding few thousand years. To verify the accuracy of the method, several artefacts that were datable by other techniques were tested; the results of the testing were in reasonable agreement with the true ages of the objects. However, in 1958, Hessel de Vries was able to demonstrate that the 14

C / 12

C ratio had changed over time by testing wood samples of known ages and showing there was a significant deviation from the expected ratio. This discrepancy, often called the de Vries effect, was resolved by the study of tree rings. [ 20 ] [ 21 ] Comparison of overlapping series of tree rings allowed the construction of a continuous sequence of tree-ring data that spanned 8,000 years. [ 20 ] (Since that time the tree-ring data series has been extended to 13,900 years.) [ 22 ] Carbon-dating the wood from the tree rings themselves provided the check needed on the atmospheric 14

C / 12

C ratio: with a sample of known date, and a measurement of the value of N (the number of atoms of 14

C remaining in the sample), the carbon-dating equation allows the calculation of N 0 – the number of atoms of 14

C in the sample at the time the tree ring was formed – and hence the 14

C / 12

C ratio in the atmosphere at that time. [ 20 ] Armed with the results of carbon-dating the tree rings, it became possible to construct calibration curves designed to correct the errors caused by the variation over time in the 14

C / 12

C ratio. [ 23 ] These curves are described in more detail below .

Atmospheric 14

C. New Zealand [ 24 ] and Austria. [ 25 ] The New Zealand curve is representative of the Southern Hemisphere; the Austrian curve is representative of the Northern Hemisphere. Atmospheric nuclear weapon tests almost doubled the concentration of 14

C in the Northern Hemisphere. [ 9 ] The date that the Partial Test Ban Treaty (PTBT) went into effect is marked on the graph.

Coal and oil began to be burned in large quantities during the 1800s. Both coal and oil are sufficiently old that they contain little detectable 14

C and, as a result, the CO

2 released substantially diluted the atmospheric 14

C / 12

C ratio. Dating an object from the early 20th century hence gives an apparent date older than the true date. For the same reason, 14

C concentrations in the neighbourhood of large cities are lower than the atmospheric average. This fossil fuel effect (also known as the Suess effect, after Hans Suess. who first reported it in 1955) would only amount to a reduction of 0.2% in 14

C activity if the additional carbon from fossil fuels were distributed throughout the carbon exchange reservoir, but because of the long delay in mixing with the deep ocean, the actual effect is a 3% reduction. [ 20 ] [ 26 ]

A much larger effect comes from above-ground nuclear testing, which released large numbers of neutrons and created 14

C. From about 1950 until 1963, when atmospheric nuclear testing was banned, it is estimated that several tonnes of 14

C were created. If all this extra 14

C had immediately been spread across the entire carbon exchange reservoir, it would have led to an increase in the 14

C / 12

C ratio of only a few per cent, but the immediate effect was to almost double the amount of 14

C in the atmosphere, with the peak level occurring in about 1965. The level has since dropped, as the "bomb carbon" (as it is sometimes called) percolates into the rest of the reservoir. [ 20 ] [ 26 ] [ 27 ]

Isotopic fractionation [ edit ]

Photosynthesis is the primary process by which carbon moves from the atmosphere into living things. In both photosynthetic pathways (C3 and C4 ) 12

C is absorbed slightly more easily than 13

C. which in turn is more easily absorbed than 14

C ratios in plants that differ from the ratios in the atmosphere. This effect is known as isotopic fractionation. [ 28 ] [ 29 ]

To determine the degree of fractionation that takes place in a given plant, the amounts of both 12

C and 13

C isotopes are measured, and the resulting 13

C / 12

C ratio is then compared to a standard ratio known as PDB. [ note 5 ] The 13

C / 12

C ratio is used instead of 14

C / 12

C because the former is much easier to measure, and the latter can be easily derived: the depletion of 13

C relative to 12

C is proportional to the difference in the atomic masses of the two isotopes, so the depletion for 14

C is twice the depletion of 13

C. [ 12 ] The fractionation of 13

C. known as ? 13 C. is calculated as follows: [ 28 ]

where the ‰ sign indicates parts per thousand. [ 28 ] Because the PDB standard contains an unusually high proportion of 13

C. [ note 6 ] most measured ? 13 C values are negative.

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I have found the man of my dreams - thank you.

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Dating 60 plus

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Expectations

Make sure that you don't expect too much from the men you date. All women want a Lothario who is tall, handsome and successful, but most single men in their 60s have allowed their housekeeping skills to deteriorate and many have paunches and less hair on their heads than they once did. Also, men become more set in their ways. Before your first attempt at the dating scene, make up you mind what's important in a man; and above all, be realistic.

Act Naturally

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Wednesday, 26 February 2014

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Online dating service

From Wikipedia, the free encyclopedia

Online dating ( OD ) or Internet dating is a personal introductory system whereby individuals can find and contact each other over the Internet to arrange a date. usually with the objective of developing a personal, romantic, or sexual relationship. Online dating services usually provide unmoderated matchmaking over the Internet. through the use of personal computers or cell phones. Users of an online dating service would usually provide personal information, to enable them to search the service provider's database for other individuals. Members use criteria other members set, such as age range, gender and location.

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Justine, 2014-04-20

Thank you Telegraph Dating. My first experience of online dating. Met the man of my dreams on this site - the first guy I chatted to & the only guy I dated. I hope to spend the rest of my life with this wonderful man. Thank you for helping us find each other X

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Guardian Soulmates

If you're looking for love you've come to the right place: welcome to Soulmates, the Guardian's online dating service. We offer dating services to all, including straight and gay dating. lesbian dating. dating for professionals, dating in London. and UK dating. Visit the Soulmates blog for dating tips and more information.

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