Factors controlling the spatial variability of soil aggregates and associated organic carbon across a semi-humid watershed

  • Pingping Zhang
  • , Yunqiang Wang
  • , Lan Xu
  • , Hui Sun
  • , Ruijie Li
  • , Jingxiong Zhou

Research output: Contribution to journalArticlepeer-review

31 Scopus citations

Abstract

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.

Original languageEnglish
Article number151155
JournalScience of the Total Environment
Volume809
DOIs
StatePublished - 25 Feb 2022
Externally publishedYes

Keywords

  • Aggregate stability
  • Carbon fraction
  • Carbon sequestration
  • Carbon stability
  • Loess Plateau
  • Structural equation modelling

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