Dinosaur eggs dating back 130 million years discovered by Chinese builders

Thanks for reading, especially if you read the whole thing! Matt Matt Herod October 1, Cherrenekoff radiation is a pretty way to demonstrate radiation. Sorry my own contribution is so slow in coming…it has been a busy month PhD wise. Anyway, in the call for posts I said: For this wedge the topic will be momentous discoveries in geology or its sub-disciplines that you feel have altered or shaped our understanding of how the Earth works, or opened new doors into research that had never been considered before. The discovery you choose does not have to be universally recognized as momentous but should be in your opinion. It could be something that we take for granted every day, but is in actuality part of the underpinnings of our science. The discovery I am going to discuss is one that a wide variety of different geoscience disciplines uses every day and one that is particularly near and dear to my heart, since my PhD. The consequences of the discovery of radioactivity have been extremely far reaching in many fields, particularly the geosciences.

Soil and Groundwater Sampling & Laboratory Services

At the time that Darwin’s On the Origin of Species was published, the earth was “scientifically” determined to be million years old. By , it was found to be 1. In , science firmly established that the earth was 3.

The Ambient Groundwater Monitoring and Assessment (GAMA) program, sponsored by the California The large volume of old groundwater observed in these wells is not likely to have carried advectively transported post-modern contaminants. The semi-confined aquifers that comprise the basin (VOCs), and groundwater age dating (using the tritium.

IAEA CRP at a Glance The increasing global water demand for agriculture, domestic and industrial uses, combined with the impact of pollution and climate change on surface waters, is forcing local water authorities to rely more and more on groundwater. Shallow aquifers, containing groundwater recently recharged, are initially used in first instance, often in a conjunctive manner with water supply sources derived from rivers or lakes. However, intense exploitation of these shallow aquifer systems often leads to important lowering of the water tables, water quality deterioration, soil subsidence and other environmental impacts.

Exploration and exploitation of deeper aquifer systems, containing older groundwater, probably recharged thousands of years ago or at distant areas, is often the next option used as a source of water. A proper understanding of the origin, history and dynamics of old groundwaters found in deep aquifers is a key pre-requisite for the assessment of the reliability and potential of these resources as a major source of water supply in medium and long-terms. Recent breakthrough developments in analytical methods e.

Bristlecone Pines

In those regions, elevated nitrate concentrations put additional pressure on the scarce water resources, as they pose a serious health risk. This study applies a multidisciplinary approach hydrogeology, isotope hydrology, and geochemistry to understand the origin and fate of nitrate in groundwater of the semi-arid Kalahari of Botswana.

Our investigations suggest that nitrate in groundwater of the study area is of natural origin, leached from a pool in the unsaturated zone that was actively involved in the soil nitrogen cycle. The presence of active minor recharge was found, showing that nitrate may be transported into the groundwater under the present conditions. Yet, slow travel times of replenishing water and the low recharge amounts render the thick unsaturated zone into a long-term reservoir for nitrate.

Sources of chloride and implications for 36Cl dating of old groundwater, southwestern Great Artesian Basin, Australia.

Advertisement Over the past several decades, U. No company would be allowed to pour such dangerous chemicals into the rivers or onto the soil. But until recently, scientists and environmental officials have assumed that deep layers of rock beneath the earth would safely entomb the waste for millennia. There are growing signs they were mistaken. Records from disparate corners of the United States show that wells drilled to bury this waste deep beneath the ground have repeatedly leaked, sending dangerous chemicals and waste gurgling to the surface or, on occasion, seeping into shallow aquifers that store a significant portion of the nation’s drinking water.

In , contaminants from such a well bubbled up in a west Los Angeles dog park. Within the past three years, similar fountains of oil and gas drilling waste have appeared in Oklahoma and Louisiana. In South Florida, 20 of the nation’s most stringently regulated disposal wells failed in the early s, releasing partly treated sewage into aquifers that may one day be needed to supply Miami’s drinking water.

There are more than , underground waste and injection wells nationwide, more than , of which shoot industrial fluids thousands of feet below the surface. Scientists and federal regulators acknowledge they do not know how many of the sites are leaking. Federal officials and many geologists insist that the risks posed by all this dumping are minimal. Accidents are uncommon, they say, and groundwater reserves — from which most Americans get their drinking water — remain safe and far exceed any plausible threat posed by injecting toxic chemicals into the ground.

Radiometric dating

The Sun-flag Hi-no-Maru consists of a red circle on a white background. The metric system is the legal standard. The total area of Japan is , sq km , sq mi. Comparatively, the area occupied by Japan is slightly smaller than the state of California.

Dating of Groundwater with Isotope. Download. For long-term potential of these isotopes can resource management decisions, and old water, for example, then it is mining Isotopes of a particular element have the and photons and lower-energy cosmic process studies within a groundwater complicate interpretation, but can often climate.

The Radiocarbon Revolution Since its development by Willard Libby in the s, radiocarbon 14C dating has become one of the most essential tools in archaeology. Radiocarbon dating was the first chronometric technique widely available to archaeologists and was especially useful because it allowed researchers to directly date the panoply of organic remains often found in archaeological sites including artifacts made from bone, shell, wood, and other carbon based materials.

In contrast to relative dating techniques whereby artifacts were simply designated as “older” or “younger” than other cultural remains based on the presence of fossils or stratigraphic position, 14C dating provided an easy and increasingly accessible way for archaeologists to construct chronologies of human behavior and examine temporal changes through time at a finer scale than what had previously been possible. The application of Accelerator Mass Spectrometry AMS for radiocarbon dating in the late s was also a major achievement.

Compared to conventional radiocarbon techniques such as Libby’s solid carbon counting, the gas counting method popular in the mid s, or liquid scintillation LS counting, AMS permitted the dating of much smaller sized samples with even greater precision. Regardless of the particular 14C technique used, the value of this tool for archaeology has clearly been appreciated. However, as with any dating technique there are limits to the kinds of things that can be satisfactorily dated, levels of precision and accuracy, age range constraints, and different levels of susceptibility to contamination.

Probably the most important factor to consider when using radiocarbon dating is if external factors, whether through artificial contamination, animal disturbance, or human negligence, contributed to any errors in the determinations. For example, rootlet intrusion, soil type e. Bioturbation by crabs, rodents, and other animals can also cause samples to move between strata leading to age reversals.

Shell may succumb to isotopic exchange if it interacts with carbon from percolating ground acids or recrystallization when shell aragonite transforms to calcite and involves the exchange of modern calcite. The surrounding environment can also influence radiocarbon ages.

Isotope methods for dating old groundwater

Can you find a match? After meeting all of the contestants it will be up to you to pick your favourite and perhaps propose a second date. On your groundwater samples that is. Starting to find some answers on water chemistry of baseflow samples from the Yukon.

Groundwater dating by radio-krypton (81Kr; half-life of about , years) was applied to the sedimentary basin aquifer of the North China Plain (NCP).

Carbon dating and other cosmogenic methods The occurrence of natural radioactive carbon in the atmosphere provides a unique opportunity to date organic materials as old as roughly 60, years. Unlike most isotopic dating methods, the conventional carbon dating technique is not based on counting daughter isotopes. It relies instead on the progressive decay or disappearance of the radioactive parent with time. Newly created carbon atoms were presumed to react with atmospheric oxygen to form carbon dioxide CO2 molecules.

Radioactive carbon thus was visualized as gaining entrance wherever atmospheric carbon dioxide enters—into land plants by photosynthesis, into animals that feed on the plants, into marine and fresh waters as a dissolved component, and from there into aquatic plants and animals. In short, all parts of the carbon cycle were seen to be invaded by the isotope carbon Invasion is probably not the proper word for a component that Libby calculated should be present only to the extent of about one atom in a trillion stable carbon atoms.

So low is such a carbon level that no one had detected natural carbon until Libby, guided by his own predictions, set out specifically to measure it. His success initiated a series of measurements designed to answer two questions: Is the concentration of carbon uniform throughout the plant and animal kingdoms? After showing the essential uniformity of carbon in living material, Libby sought to answer the second question by measuring the radiocarbon level in organic samples dated historically—materials as old as 5, years from sources such as Egyptian tombs.

With correction for radioactive decay during the intervening years, such old samples hopefully would show the same starting carbon level as exists today.

UK Thermal and Mineral Springs

Tritium is still be used since it is produced in the atmosphere in small amounts and it can be measured by low-level counting or by the ingrowth of its decay product He I don’t know why the article states a large range for He I expect it is a mash-up of He-3 ingrowth from tritium decay and the subsurface production of He-4 from alpha decay of heavy radioactive elements an alpha particle is a He-4 nucleus. Thus it can be used to estimate age of very old water.

Argon would be very useful in age dating groundwater but there are currently only about 3 labs in the world who can measure it and radioactive counting needs a large volume of water.

Abstract The Milk River aquifer in southern Alberta, Canada, consists of sandstone interbedded between thick shale units. The groundwater is confined and discharges by both upward and downward leakage through the shales.

Well-known examples include those in Bath, Buxton and Harrogate. Bathing in these waters was popular amongst fashionable society in the seventeenth and eighteenth centuries, as it was considered beneficial to health. The practice continued into the nineteenth century but declined after that in the UK. Thermal springs are a natural phenomenon which occur where hot water from great depths in the Earth rises to the surface.

In the UK, groundwater normally has a temperature around oC and reflects the average annual air temperature. Shallow springs therefore have a similar temperature. As you go deeper underground the temperature increases due to heat stored in the earth, originating from when the Earth was formed and from radioactive decay of minerals. This is known as the geothermal gradient. As the temperature of the earth increases with depth, so too does the temperature of the groundwater.

The source and travel path of groundwater to springs differs and as a result the nature of the water that issues from the spring is very different. The springs in Bath, Buxton and Harrogate are used here as examples to illustrate the differences. There is some debate about the source of the water but the generally accepted hypothesis is that rain water falling on the Mendip Hills to the south of the city infiltrates the Carboniferous Limestone and flows to the north, beneath the North Somerset coal field reaching a depth of 2.

It then rises up through fractures in the Jurassic rocks beneath the city.

Paradox of groundwater age

Global warming and desertification The record from the polar ice core clearly shows that the increase in greenhouse gas concentrations in the atmosphere started with the Industrial Revolution in the eighteenth century, though the rate of increase accelerated after the middle of the twentieth century. It is the general consensus that global warming has occurred because of the increase in atmospheric concentrations of greenhouse gases due to human activities Houghton et al.

Human activities may influence local precipitation directly through changes in local vegetation cover, and indirectly through global warming. The direct influence of deforestation of the Amazonian tropical rain forest on Amazonian climate has been discussed e. Almost all research results suggest a positive feedback effect of the decrease in local evapotranspiration by deforestation on local precipitation, i.

Modeling of groundwater 14C ages using NETPATH indicates that a significant part of groundwater in the Alliston aquifer is less than 13, years old; however, older groundwater in the range of 15,–23, years is also present in the aquifer.

A prominent deflation surface at the northern lake exposes lacustrine sands Thick gray lacustrine sediments suggest a prolonged and relatively deep-water environment between 9 and 5 ka see SI Appendix, Fig. Pollen from lake sediments and 14C dating of preserved tree subfossils indicate the dominance of Betula, Picea, Abies, Pinus, and Quercus. However, during wet conditions in the early and middle Holocene, this area is characterized as temperate steppe environment, dominated by grasslands and trees near lakes and streams 8 , 10 , 12 , Well-developed dark grassland-type paleosols mollisols at the southern edge of the Hunshandake, OSL-dated to between 6.

Lacustrine sands underlying this paleosol indicate an earlier wetland environment followed by soil formation that indicates a rapid transition to dry conditions at ca. Because the southern part of the Hunshandake was not impacted by ground water sapping until recently, it returned to green conditions again at ca. Similarly, paleosols developed during the period between ca.

What is Groundwater?

Hiroshima University, Japan B. Chemical Geology, , Sturchio 81Kr dating of old groundwater.

Groundwater Geochemistry and Isotopes provides the theoretical understanding and interpretive methods and contains a useful chapter presenting the basics of sampling and analysis. This text teaches the thermodynamic basis and principal reactions involving the major ions, gases and isotopes during groundwater recharge, weathering and redox.

Paper details technique to date groundwater December 2, by Karen B. Roberts, University of Delaware A groundbreaking Nature Geoscience article co-authored by UD geochemist Neil Sturchio describes a new method to accurately date groundwater. Pictured at a well in Brazil is machinery used for the extraction of dissolved gases from groundwater. The apparatus extracts the gases as the water flows through and compresses them into a small aluminum cylinder. Knowing the age of the groundwater provides important clues about the sustainability of water resources , information that is particularly important in dry or arid climates.

The technique involves measuring Krypton , a rare isotope produced by cosmic rays in the Earth’s atmosphere. Sturchio explained that as rain is absorbed into the ground, a miniscule amount of the isotope comes with it.

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