In:
Water Resources Research, American Geophysical Union (AGU), Vol. 53, No. 7 ( 2017-07), p. 5677-5689
Abstract:
Crustal fluxes are often invoked to explain groundwater helium in excess of steady state local production The relationship between 234 U/ 238 U activity ratios and 4 He contents suggests a common process releasing 234 U and 4 He into groundwater locally Modeling 4 He release from comminuted grains after glaciation‐induced fracturing could explain local 4 He excesses in groundwater
Type of Medium:
Online Resource
ISSN:
0043-1397
,
1944-7973
DOI:
10.1002/2016WR020014
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2029553-4
detail.hit.zdb_id:
5564-5
SSG:
13
SSG:
14
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