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

被引:26
作者
Zhang, Pingping [1 ,2 ,3 ]
Wang, Yunqiang [1 ,2 ,3 ,5 ]
Xu, Lan [1 ,5 ]
Sun, Hui [1 ,4 ]
Li, Ruijie [1 ,4 ]
Zhou, Jingxiong [1 ,5 ]
机构
[1] Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, Xian 710061, Shaanxi, Peoples R China
[2] CAS Ctr Excellence Quaternary Sci & Global Change, Xian 710061, Peoples R China
[3] Natl Observat & Res Stn Earth Crit Zone Loess Pla, Xian 710061, Peoples R China
[4] Xian Inst Innovat Earth Environm Res, Xian 710061, Peoples R China
[5] Univ Chinese Acad Sci, Beijing 100049, Peoples R China
基金
中国国家自然科学基金;
关键词
Aggregate stability; Carbon stability; Carbon sequestration; Carbon fraction; Structural equation modelling; Loess Plateau; LOESS-PALEOSOL SEQUENCE; LAND-USE CHANGE; DYNAMICS; STABILITY; NITROGEN; PLATEAU; FRACTIONS; MATTER; STABILIZATION; CLIMATE;
D O I
10.1016/j.scitotenv.2021.151155
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Y 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 km(2)) 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 ecohydrological 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. (C) 2021 Elsevier B.V. All rights reserved.
引用
收藏
页数:15
相关论文
共 72 条
[1]   Vertical variations of soil water and its controlling factors based on the structural equation model in a semi-arid grassland [J].
A, Yinglan ;
Wang, Guoqiang ;
Liu, Tingxi ;
Shrestha, Sangam ;
Xue, Baolin ;
Tan, Zhongxin .
SCIENCE OF THE TOTAL ENVIRONMENT, 2019, 691 :1016-1026
[2]   Soil aggregate stability:: A review [J].
Amézketa, E .
JOURNAL OF SUSTAINABLE AGRICULTURE, 1999, 14 (2-3) :83-151
[3]   Plant- or microbial-derived? A review on the molecular composition of stabilized soil organic matter [J].
Angst, Gerrit ;
Mueller, Kevin E. ;
Nierop, Klaas G. J. ;
Simpson, Myrna J. .
SOIL BIOLOGY & BIOCHEMISTRY, 2021, 156
[4]  
[Anonymous], 2003, Joint Iraq Needs Assessment
[5]   Soil organic carbon physical fractions and aggregate stability influenced by land use in humid region of northern Iran [J].
Ayoubi, Shamsollah ;
Mirbagheri, Zahra ;
Mosaddeghi, Mohammad Reza .
INTERNATIONAL AGROPHYSICS, 2020, 34 (03) :343-353
[6]   Soil aggregation and organic carbon as affected by topography and land use change in western Iran [J].
Ayoubi, Shamsollah ;
Karchegani, Parisa Mokhtari ;
Mosaddeghi, Mohammad Reza ;
Honarjoo, Naser .
SOIL & TILLAGE RESEARCH, 2012, 121 :18-26
[7]   FIELD-SCALE VARIABILITY OF SOIL PROPERTIES IN CENTRAL IOWA SOILS [J].
CAMBARDELLA, CA ;
MOORMAN, TB ;
NOVAK, JM ;
PARKIN, TB ;
KARLEN, DL ;
TURCO, RF ;
KONOPKA, AE .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1994, 58 (05) :1501-1511
[8]   CARBON AND NITROGEN DISTRIBUTION IN AGGREGATES FROM CULTIVATED AND NATIVE GRASSLAND SOILS [J].
CAMBARDELLA, CA ;
ELLIOTT, ET .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1993, 57 (04) :1071-1076
[9]   Soil Carbon Sequestration Potential for "Grain for Green" Project in Loess Plateau, China [J].
Chang, Ruiying ;
Fu, Bojie ;
Liu, Guohua ;
Liu, Shuguang .
ENVIRONMENTAL MANAGEMENT, 2011, 48 (06) :1158-1172
[10]   Soil organic carbon stocks in Laos: spatial variations and controlling factors [J].
Chaplot, Vincent ;
Bouahom, Bounthong ;
Valentin, Christian .
GLOBAL CHANGE BIOLOGY, 2010, 16 (04) :1380-1393