In:
Global Biogeochemical Cycles, American Geophysical Union (AGU), Vol. 33, No. 7 ( 2019-07), p. 849-874
Abstract:
Common hydrological factors explain variability in riverine dissolved organic carbon and dissolved black carbon concentrations, however; Variation in soil properties, temperature, antecedent rainfall, and aerosol deposition may drive divergence in their relative abundance At an unprecedented geographic scale, we find that aerosol BC contributes significantly to riverine fluxes of DBC
Type of Medium:
Online Resource
ISSN:
0886-6236
,
1944-9224
DOI:
10.1029/2018GB006140
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2019
detail.hit.zdb_id:
2021601-4
SSG:
12
SSG:
13
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