TY - JOUR
T1 - Factors controlling the spatial variability of soil aggregates and associated organic carbon across a semi-humid watershed
AU - Zhang, Pingping
AU - Wang, Yunqiang
AU - Xu, Lan
AU - Sun, Hui
AU - Li, Ruijie
AU - Zhou, Jingxiong
N1 - Publisher Copyright:
© 2021 Elsevier B.V.
PY - 2022/2/25
Y1 - 2022/2/25
N2 - Soil aggregates (SA) play crucial roles in soil organic carbon (SOC) sequestration. Different SA fractions contribute differently to the sequestration of SOC. However, few studies have examined the factors controlling SA fractions and associated SOC contents across a watershed. Soil samples were collected at 0–10 cm (surface layer) and 10–20 cm (subsurface layer) from 88 sites across a semi-humid watershed (1.1 km2) on the Loess Plateau, China. These samples were separated into macroaggregates (MA), microaggregates (MI), and silt + clay fractions (SC) by wet-sieving, and SOC content of each fraction was determined. The objectives were to: 1) investigate the spatial variability of SA fractions and associated SOC contents as well as their main controls across an entire watershed, and 2) explore the linkages between soil aggregation and SOC sequestration. The bulk and aggregate SOC contents of all SA fractions showed moderate variability, with coefficient of variations of 23.3–31.9%. Geostatistical analysis indicated that the spatial patterns of SA fractions and SOC content varied with aggregate size. From combined Spearman's correlation analysis and structural equation modelling, we found that soil texture was an important control on the spatial variability of all SA fractions and associated SOC contents. Vegetation dynamics and management practices associated with land use were also important controls on MA and MI and their associated SOC contents, especially in the surface layer. However, SC and its associated SOC content were more sensitive to eco-hydrological processes related to topography. Among the land uses, grassland had the greatest SOC sequestration potential. The fine roots of herbs can wrap MI in MA and increase SOC content within MA, which is the primary mechanism responsible for SOC sequestration in grasslands. These results indicate that using vegetation with fine root systems for restoration is a good strategy to increase SOC sequestration in this region.
AB - Soil aggregates (SA) play crucial roles in soil organic carbon (SOC) sequestration. Different SA fractions contribute differently to the sequestration of SOC. However, few studies have examined the factors controlling SA fractions and associated SOC contents across a watershed. Soil samples were collected at 0–10 cm (surface layer) and 10–20 cm (subsurface layer) from 88 sites across a semi-humid watershed (1.1 km2) on the Loess Plateau, China. These samples were separated into macroaggregates (MA), microaggregates (MI), and silt + clay fractions (SC) by wet-sieving, and SOC content of each fraction was determined. The objectives were to: 1) investigate the spatial variability of SA fractions and associated SOC contents as well as their main controls across an entire watershed, and 2) explore the linkages between soil aggregation and SOC sequestration. The bulk and aggregate SOC contents of all SA fractions showed moderate variability, with coefficient of variations of 23.3–31.9%. Geostatistical analysis indicated that the spatial patterns of SA fractions and SOC content varied with aggregate size. From combined Spearman's correlation analysis and structural equation modelling, we found that soil texture was an important control on the spatial variability of all SA fractions and associated SOC contents. Vegetation dynamics and management practices associated with land use were also important controls on MA and MI and their associated SOC contents, especially in the surface layer. However, SC and its associated SOC content were more sensitive to eco-hydrological processes related to topography. Among the land uses, grassland had the greatest SOC sequestration potential. The fine roots of herbs can wrap MI in MA and increase SOC content within MA, which is the primary mechanism responsible for SOC sequestration in grasslands. These results indicate that using vegetation with fine root systems for restoration is a good strategy to increase SOC sequestration in this region.
KW - Aggregate stability
KW - Carbon fraction
KW - Carbon sequestration
KW - Carbon stability
KW - Loess Plateau
KW - Structural equation modelling
UR - https://www.scopus.com/pages/publications/85117965770
U2 - 10.1016/j.scitotenv.2021.151155
DO - 10.1016/j.scitotenv.2021.151155
M3 - 文章
C2 - 34688765
AN - SCOPUS:85117965770
SN - 0048-9697
VL - 809
JO - Science of the Total Environment
JF - Science of the Total Environment
M1 - 151155
ER -