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Tytuł pozycji:

Changes in soil aggregate stability and aggregate-associated organic carbon during old-field succession in karst valley.

Tytuł:
Changes in soil aggregate stability and aggregate-associated organic carbon during old-field succession in karst valley.
Autorzy:
Li Y; School of Geographical Sciences, Southwest University, Chongqing, 400715, China. .
Yu P; School of Geographical Sciences, Southwest University, Chongqing, 400715, China. .; Chongqing Jinfo Mountain Karst Ecosystem National Observation and Research Station, Tiansheng Road, Chongqing, 400715, China. .
Shen L; School of Geographical Sciences, Southwest University, Chongqing, 400715, China.
Źródło:
Environmental monitoring and assessment [Environ Monit Assess] 2021 Dec 08; Vol. 194 (1), pp. 15. Date of Electronic Publication: 2021 Dec 08.
Typ publikacji:
Journal Article
Język:
English
Imprint Name(s):
Publication: 1998- : Dordrecht : Springer
Original Publication: Dordrecht, Holland ; Boston : D. Reidel Pub. Co., c1981-
MeSH Terms:
Carbon*/analysis
Soil*
China ; Ecosystem ; Environmental Monitoring ; Forests ; Humans
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Grant Information:
SWU019024 Fundamental Research Funds for the Central Universities in China; SWU019023 Fundamental Research Funds for the Central Universities in China; 42171175 National Natural Science Foundation of China
Contributed Indexing:
Keywords: Abandoned farmland; Rehabilitated land; Soil organic carbon; Southwest China; Water-stable aggregates
Substance Nomenclature:
0 (Soil)
7440-44-0 (Carbon)
Entry Date(s):
Date Created: 20211209 Date Completed: 20211210 Latest Revision: 20211214
Update Code:
20240105
DOI:
10.1007/s10661-021-09662-2
PMID:
34881406
Czasopismo naukowe
Soil is the largest carbon pool whose change will have an impact on the terrestrial carbon cycle in the terrestrial ecosystem. Old-field succession on abandoned farmland, which usually has a noticeable effect on soil status, is a common phenomenon in karst valley where human activity alters frequently. In order to understand the changes in the accumulation of organic carbon (OC) in aggregates and bulk soil in different stages of old-field succession on abandoned farmland in the karst valley area, soil samples were collected at 0-10-cm and 10-20-cm depth representing three typical stages of old-field succession, i.e., abandoned farmland, secondary grass, and secondary shrub in Qingmuguan karst valley area, Chongqing City, Southwest China. Results displayed that during old-field succession (1) the mean weight diameter and geometric mean diameter of the aggregates increased and the fractal dimension decreased; (2) OC content within aggregates and bulk soil had no significant change in topsoil (0-10 cm); OC content within microaggregates and bulk soil had a significant reduction in subsoil (10-20 cm); the OC content within silt and clay fractions was significantly higher than that within the other two kinds of aggregates; (3) bulk-soil OC storage had no significant change but its accumulation relied more on the increase in the number of larger aggregates. It is concluded that the old-field succession in karst valley was beneficial to protect against soil erosion by improving soil aggregate stability, but had a limited effect on soil organic carbon sequestration.
(© 2021. The Author(s), under exclusive licence to Springer Nature Switzerland AG.)

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