In:
Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 35, No. 12 ( 2021-12)
Abstract:
The H 2 soil uptake is driven by the temporal dynamics of soil moisture Considering the soil dry‐wet sequences may improve the global estimates of the H 2 soil sink Global distribution of biotic and abiotic limitations to H 2 uptake are presented
Type of Medium:
Online Resource
ISSN:
0886-6236
,
1944-9224
DOI:
10.1029/2021GB006987
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2021
detail.hit.zdb_id:
2021601-4
SSG:
12
SSG:
13