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profile samples for dating sites

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Another indication of scam is mass-mailing everybody on the site. Basically, the point of all this is that we would like to be able to measure elevations with better than 10 m precision. On the plus side, your profile is available only to OkCupid users who are signed in to the site.

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If you are reading this, you are probably familiar with the two-nuclide diagram commonly used to represent paired Be and Al data:. This example is from a review article by Darryl Granger from in GSA Special Paper that gives a good description of what the diagram is and how it is supposed to work.

In certain manifestations of this diagram primarily when plotted with a log x-axis and a linear y-axisthe simple exposure region vaguely resembles a banana, for example:. The lines are contours of burial time in Myr. So these samples have been buried for 2. This is the foundation of the method of cosmogenic-nuclide burial dating. The problem arises when other nuclides are involved.

So, again, exposure goes to the right and burial goes down. This figure has a lot of data in it that are beside the point from the perspective of this post, but the point is that it has the opposite axes: Thus, exposure still goes to the right at least for a whilebut burial goes UP.

US researchers generally plot [Ne] vs. So the question here is which one to use. I have a pretty clear opinion on this. Thus, I advocate always plotting the longer-lived nuclide of the pair on the x-axis, and the ratio of the shorter-lived to longer-lived nuclide on the y-axis.

Then burial always goes down, as we expect. Of course, I am in the US, but I am not just cheering for my own team here. It really does make more sense for two-nuclide diagrams to always behave the same way no matter what nuclide pair is involved. This post is about elevation measurements for exposure-dating samples, and how accurate they need to be. Basically, the main thing that controls cosmogenic-nuclide production rates is site elevation, or, more precisely, atmospheric pressure — at higher elevation, there is less atmosphere between you and the extraterrestrial cosmic-ray flux, so the production rate is higher.

Thus, to compute the cosmogenic-nuclide production rate at a sample site, the first thing we need to know is the elevation. Once we know the elevation, we can convert it to a mean atmospheric pressure using a model for how the atmospheric pressure varies with elevation, and then compute the production rate. The second one — converting an elevation to a mean atmospheric pressure during the exposure duration of the sample — is actually a fairly complicated problem and is the subject of another postas well as a fairly large number of papers.

However, the first one — accurately measuring the elevation — ought to be pretty simple. In general, determining your elevation is a fairly well-established technology that people have been working on for centuries.

So the rest of this post covers i exactly how precise we need elevation measurements to be, and ii various ways to accomplish or not accomplish that goal. So how precise do we need elevation measurements to be? Basically, the point of all this is that we would like to be able to measure elevations with better than 10 m precision. Preferably quite a lot better. Note, however, that this condition dates back only to approximately the year Prior to that time, the GPS satellite network, which of course was operated by the U.

So handheld GPS data from that era are much less accurate, with horizontal precision in the tens-of-meters range. Unfortunately, in nearly all cases the vertical accuracy of a GPS position is not nearly as good as its horizontal accuracy. This is just because GPS profiles are mostly not right over your head, but well away from the zenith at shallow angles toward the horizon. A rough rule of thumb is that vertical position errors are usually about twice horizontal ones, so if your handheld GPS is indicating m horizontal precision, that is something like m vertical precision.

So in general, this is pretty good: There are, however, a couple of other important points about these data. One, they both show an offset in which the handheld measurement is systematically approx. I suspect this may reflect my error in converting between ellipsoid and geoid heights more about this later for the two sets of measurements: Two, there are some pretty serious outliers in the m range — sometimes the measurement is very wrong.

These data are from Antarctica, which is i remote, and ii cold. Item i means you are highly motivated to conserve battery power because you have only a finite supply of AA batteries in your camp, and item ii means you are highly motivated to complete the measurement quickly and put your mittens back on.

The next question, then, is how to do better. There are for strategies for this. One is just to buy a more expensive dual-frequency GPS that can be differentially corrected. Still, a suitable unit can usually be borrowed from most university geoscience departments.

However, this solution creates a number of new problems. One is weight — if your fieldwork is foot-supported, you have just added a lot of weight to your pack. Another is power — most of these units require daily recharging or heavy gel-cells. Again, a potential problem for remote fieldwork. A third potential problem is that if you are operating someplace very remote like Antarctica, againyou will not be within range of stationary GPS stations that can be used for differential correction, so you will need to not only carry a rover unit with you to the sample sites, but also establish a temporary base station at your camp with a second unit.

A fourth is that you need to learn enough about GPS data processing to not make errors in the processing that are much worse than you would have made with the inexpensive unit.

This is a serious consideration. A final problem is that collecting enough data with a Trimble DGPS unit to eventually yield submeter site precision takes a while — generally on the order of 30 minutes per site. Doing this at each site would seriously limit the number of samples that could be collected in a day.

A completely different strategy is to measure sample elevations using a barometer or barometric altimeter. Of course, in this example in most cases you will find that you could have just plotted your horizontal GPS position on the map and read off the contour elevation to get the same result.

This strategy does require a fancy GPS unit, but it is fast because you only need to do a couple of min occupations per day and light because you can minimize carrying around the heavy antenna and batteries. Summarizing the discussion up to now, a decent-quality handheld GPS is just barely good enough for exposure dating in that errors in elevations measured using this method transfer to 0.

If you can, though, you should do better, either with a more elaborate GPS unit or some combination of DGPS benchmarks and barometric survey. There is, however, one final topic on the subject of GPS measurements of sample elevations, that is important. What we actually want to measure for exposure dating is the elevation of a sample with respect to sea level. Elevation-atmospheric pressure models are indexed to the bottom of the atmosphere, which is sea level, so we need to know how far above sea level we are.

However, for GPS data reduction it is common to work not in a sea-level reference frame but in an ellipsoidal reference frame in which the Earth is represented by a simplified ellipsoid rather than the somewhat lumpy shape of the actual surface of the ocean generally referred to as the geoid. In some parts of the Earth they are quite different: The details are beyond the scope of this post, but the point is that a GPS elevation computed with respect to an ellipsoid is not a sea level elevation, and can be tens of meters different from the correct sea level elevation.

This works great if you know what P is. So to summarize, if we want to estimate production rates everywhere globally, we do that by formulating a scaling model and then fitting the scaling model to measured production rate calibration data. This also allows us to evaluate scaling models by asking whether they fit the calibration data, or not. So the question is, do we have production rate calibration data that span the entire useful part of production rate scaling space?

We certainly have a lot of production rate calibration data: In the world map, the size of the circles indicates the number of different samples collected at each site. From left to right, they show the distribution in latitude a simple proxy for position in the magnetic field and elevation for Be redAl greenand He-3 gray calibration data. In these plots, the size of the circle reflects how many measurements of the respective nuclides were made at each site. This shows that the available calibration data do span a wide range in latitude.

They do span a wide range in elevation. But their distribution across scaling space is not even close to uniform. Rather, with the exception of a couple of He-3 calibration sites near sea level at low latitude, latitude and elevation are highly correlated for these sites, such that they nearly all lie in a fairly narrow zone of scaling space that is at high elevation at low latitude, and at low elevation at high latitude.

The opposite corners of scaling space — high-elevation-high-latitude and low-elevation-low-latitude — are nearly empty. To figure out why, consult the following figure from a well-known article in Scientific American by George Denton and Wally Broecker. Thus, the very non-uniform distribution of calibration data in scaling space just reflects the fact that most calibration data are from glacial deposits formed during or after the LGM, and these deposits, by nature, are lower in polar regions and higher in tropical regions.

Here are the locations of Be and Al calibration data pasted onto the Denton-Broecker diagram:. Again, the main exceptions are in the He-3 data set not shown here; see abovewhere there are a few sites that consist of dated lava flows or other volcanics at low elevation and low latitude.

So, in fact, the production rate calibration data that we have, although fairly abundant now, are not, in fact, very evenly distributed across scaling space. The next question is, do we care?

For us to care, two things need to be true. Do we want to do this? Consider what is by far the most common application of exposure-dating, which is, of course, dating glacial deposits. For the most part, the places where we want to actually apply exposure-dating to glacial deposits are located very close in scaling space to the calibration data that we have.

However, there are some exceptions. So the first requirement for whether or not we care about the restricted distribution of calibration data is, in fact, met. We definitely want to exposure-date things in datings of scaling space that are empty of calibration data. We have scaling models that predict the variation in production rates everywhere in scaling space, not just near the calibration data. So the sample is, do we know that the scaling models are accurate in unsampled parts of scaling space, in particular at high latitude near the poles?

One alternative, but much less satisfying, way to answer the question is to ask whether different scaling models predict the same production rates for this region, or not.

Here is a comparison of production rate estimates for high latitude derived using the two most au courant scaling methods: Left panel shows the predicted production rates at high latitude using an Antarctic atmosphere approximation for the St blue and LSDn red scaling models; right panel shows the ratio of the two production rates.

At low elevation, both scaling models predict production rates that are within a few percent of each other because they are both pinned to calibration data at relatively low elevations at relatively high latitudesbut the predictions diverge at higher elevations. At m in Antarctica, LSDn scaling predicts ca. This is a pretty big difference.

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I have no idea! This is NOT an advertising. This post is about elevation measurements for exposure-dating samples, and how accurate they need to be. Basically, the main thing that controls cosmogenic-nuclide production rates is site elevation, or, more precisely, atmospheric pressure — at higher elevation, there is less atmosphere between you and the extraterrestrial cosmic-ray . Table 2 La Boja.

Radiocarbon dating results. Calibration used Calib against IntCal13 (Stuiver and Reimer, ; Reimer et al., ). Unless otherwise stated, samples were ABA-pretreated. The details are beyond the scope of this post, but the point is that a GPS elevation computed with respect to an ellipsoid is not a sea level elevation, and can be tens of meters different from the correct sea level elevation. A couple of points about this:.

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    Or maybe they use some absolutely weird translator that translates the phrase like that? If you can, though, you should do better, either with a more elaborate GPS unit or some combination of DGPS benchmarks and barometric survey. A final problem is that collecting enough data with a Trimble DGPS unit to eventually yield submeter vertical precision takes a while — generally on the order of 30 minutes per site. Of course, I am in the US, but I am not just cheering for my own team here.

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    Like this typical scammy profile description: One is just to buy a more expensive dual-frequency GPS that can be differentially corrected. Launched in , the site had just over 10 million unique monthly visitors in November , according to Statista. Best Dating Sites By:

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    By far the biggest pain in the neck in the overall field of cosmogenic-nuclide geochemistry is the need to compute nuclide production rates due to muon interactions. The web service requests, which comprise the vast majority of usage, reflect the fact that the version 3 code is the back end for the antarctica. So this should be a decent approximation of how much actual use is happening. I have a pretty clear opinion on this. Your expert profile writer will create an irresistible new profile from scratch from your answers.

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