Changes in carbon and nitrogen in soil particle-size fractions along a grassland restoration chronosequence in northern China

被引:79
作者
He, Nianpeng [1 ,2 ]
Wu, Ling [1 ]
Wang, Yuesi [2 ]
Han, Xingguo [1 ]
机构
[1] Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, LAPC, Beijing 100029, Peoples R China
基金
中国国家自然科学基金;
关键词
C:N ration; Grazing exclusion; Particle-size fraction; Semiarid grassland; Carbon; ORGANIC-MATTER DYNAMICS; LAND-USE CHANGE; INNER-MONGOLIA; MANAGEMENT; STORAGE; TEXTURE; STEPPE; STOCKS; POOLS; CLAY;
D O I
10.1016/j.geoderma.2009.02.004
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Grazing exclusion (GE) can increase the carbon (C) storage of semiarid grasslands in China; however, little is known about the effect of long-term GE on the C storage of soil fractions. On the basis of a chronosequence of grassland restoration from free grazing (FG) to 28-year GE, we investigated the dynamics of total C and N in soil fractions in order to assess the impact of long-term GE on the soil fractions. The results revealed that long-term GE had a marked impact on soil particle-size fractions and their total C and N concentrations. The C associated with sand and clay in the 0-10 cm soil layer exhibited a significant logarithmic increase as period of GE increases. The increase in C storage with the introduction of GE was considerable, especially in the sand and clay fraction of 0-10 cm soil layer. The C:N ratios of the whole soil and of the sand and silt increased significantly with grassland restoration. Considering the accumulation of total C in the whole soil and soil fractions and their logarithmic increase during the GE chronosequence, we suggest that by implementing GE, the temperate grasslands of northern China could facilitate significant C storage on decade scales: however, when subjected to GE for 2 decades or more, these grassland soils would have a lower potential to further accumulate the C newly derived from litter and dead roots. (C) 2009 Elsevier B.V. All rights reserved.
引用
收藏
页码:302 / 308
页数:7
相关论文
共 40 条
[1]   Carbon, nitrogen, and sulfur pools in particle-size fractions as influenced by climate [J].
Amelung, W ;
Zech, W ;
Zhang, X ;
Follett, RF ;
Tiessen, H ;
Knox, E ;
Flach, KW .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1998, 62 (01) :172-181
[2]   CARBON TURNOVER IN SOIL PHYSICAL FRACTIONS [J].
BUYANONOVSKY, GA ;
ASLAM, M ;
WAGNER, GH .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1994, 58 (04) :1167-1173
[3]   Characterization of soil organic matter in different particle-size fractions in humid subalpine soils by CP/MAS 13C NMR [J].
Chen, JS ;
Chiu, CY .
GEODERMA, 2003, 117 (1-2) :129-141
[4]  
Chen Z., 2000, TYPICAL STEPPE ECOSY
[5]  
Christensen B.T., 1992, Advances in Soil Science, V20, P1, DOI DOI 10.1007/978-1-4612-2930-8_1
[6]   Physical fractionation of soil and structural and functional complexity in organic matter turnover [J].
Christensen, BT .
EUROPEAN JOURNAL OF SOIL SCIENCE, 2001, 52 (03) :345-353
[7]  
Conant RT, 2001, ECOL APPL, V11, P343, DOI 10.1890/1051-0761(2001)011[0343:GMACIG]2.0.CO
[8]  
2
[9]   Short-term changes in C and N distribution in soil particle size fractions induced by agricultural practices in a cultivated volcanic soil from Mexico [J].
Covaleda, Sara ;
Pajares, Silvia ;
Gallardo, Juan F. ;
Etchevers, Jorge D. .
ORGANIC GEOCHEMISTRY, 2006, 37 (12) :1943-1948
[10]   Management intensity affects density fractions of soil organic matter from grazed bahiagrass swards [J].
Dubeux, J. C. B., Jr. ;
Sollenberger, L. E. ;
Comerford, N. B. ;
Scholberg, J. M. ;
Ruggieri, A. C. ;
Vendramini, J. M. B. ;
Interrante, S. M. ;
Portier, K. M. .
SOIL BIOLOGY & BIOCHEMISTRY, 2006, 38 (09) :2705-2711