Chlorine 36 Dating Groundwater

Chlorine 36 Dating Groundwater




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PDF CHLORINE-36 DATING OF OLD GROUNDWA TER Fred M . Phillips . . .
Application of chlorine-36 technique in determining the . . .
Chlorine-36 dating of deep groundwater from northern . . .
Application of chlorine-36 technique in determining the . . .
Chlorine 36 dating of very old groundwater: 1 . The Great . . .
Chlorine 36 Dating of Very Old Groundwater: 3 . Further . . .
Chlorine 36 Dating of Very Old Groundwater: 3 . Further . . .
Chlorine-36 dating of old groundwater . Chapter 6|INIS
Application of the chlorine-36 method for the delineation . . .
PDF Chlorine Isotopes and their Application to Groundwater . . .
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www .ees .nmt .eduΒ β€ΊΒ outside β€Ί courses β€Ί hyd558 β€Ί downloads β€Ί Set_12_36Cl β€Ί Phillips_Cl-36_09-09 .pdf
Basic Principles of 36Cl Chlorine-36 has been widely used for dating old groundw ater . The 36Cl used for this purpose is produced in the atmosphere by the interaction of cosmic rays with argon atoms . The 36Cl then mixes with ordinary atmospheric chloride (mostly derived from the ocean) .
Dating based on a 36 Cl bomb pulse may be more reliable and sensitive for groundwater recharged before 1975, back as far as the mid-1950s . The above 36 Cl background concentration was deduced by determining the background-corrected Dye-3 ice core data from the frozen Arctic data, according to the estimated total 36 Cl resources .
Chlorine-36 , with its long half-life (301,000 a), is a good candidate to obtain information about residence time of C .I . groundwater . Some 36 Cl measurements were performed for groundwater dating in the Great Oriental Erg as early as 1985 ( Fontes et al ., 1985 , Guendouz, 1985 , Michelot et al ., 1989a ) .
Dating based on a (36)Cl bomb pulse may be more reliable and sensitive for groundwater recharged before 1975, back as far as the mid-1950s . The above (36)Cl background concentration was deduced by determining the background-corrected Dye-3 ice core data from the frozen Arctic data, according to the estimated total (36)Cl resources .
Chlorine 36 has many advantages as a dating tool for very old groundwater . These advantages include a suitable half-life (3 .01 Γ— 10 5 years), simple geochemistry, conservative behavior in groundwater , and a general absence of subsurface sources at levels comparable to the atmospheric input . Recent advances in tandem accelerator mass spectrometry . . .
The results confirm that the chemically distinct western GAB operates as a separate flow system with its own recharge area and its own geochemical evolution . The results indicate an area of groundwater with relatively young 36 Cl ages in the central portion of the basin which cannot be explained by flow or mixing along the presently known flow lines . It is hypothesized that an additional source of young water originated from the basin margin region to the north and northwest between the . . .
The results indicate an area of groundwater with relatively young 36 Cl ages in the central portion of the basin which cannot be explained by flow or mixing along the presently known flow lines . It is hypothesized that an additional source of young water originated from the basin margin region to the north and northwest between the Simpson Desert and Mount Isa .
Chlorine-36 has been widely used for dating old groundwater . The 36 Cl used for this purpose is produced in the atmosphere through the interaction of cosmic rays with argon atoms . The 36 Cl then mixes with ordinary atmospheric chloride (mostly d
to evaluate by direct calibration the 36 Cl production and fallout rates as important factors for the dating of deep groundwater (Balderer and Synal 1996, 1997) . Origin of chlorine-36 in groundwater 36 Cl, with a half-life of about 301,000 years, is one of the most promising isotopes for environmental studies .
Chlorine-36 is a useful isotopic tracer for determining the residence time of groundwater , identifying mixing of groundwaters and determining the characteristics of water-rock interaction . Interpreting 36Cl data in terms of water residence time* requires understanding the origin of chloride ion dissolved in the water . Groundwater age can be
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