FANG Huajun, YANG Xueming, ZHANG Xiaoping . Effect of Soil Erosion on Soil Organic Carbon in Cropland Landscape[J]. PROGRESS IN GEOGRAPHY, 2004 , 23(2) : 77 -87 . DOI: 10.11820/dlkxjz.2004.02.010

[1] Lal R. Soil erosion and the global carbon budget.Environment international,2003,29: 437~450.

[2] Schimel D S, House J I, Hibbard K A, et al. Recent patterns and mechanisms of carbon exchange by terrestrial ecosystems. Nature, 2001, 414:169~72.

[3] Pacala S W, Hurtt G C, Baker D, et al. Consistent land- and atmospherebased U.S. carbon sink estimates. Science, 2002, 292: 2316~23.

[4] Hurtt G C, Pacala S W, Moorcroft P R, Caspersen J, Shevliakova E, Houghton RA, et al. Projecting the future of the U.S. carbon sink. Proc Natl Acad Sci U S A, 2002,99:1389 ~1394.

[5] Myneni R B, Dong J, Tucker C J, Kaufmann R K, Kauppi P E, Liski J, et al. A large carbon sink in the woody biomass of northern forests. Proc. Natl. Acad. Sci. USA., 98(26):14784 ~ 14789.

[6] IPCC. Land Use, Land Use Change and Forestry. Cambridge University Press, UK. 2000

[7] Walling D E, Webb B W. Erosion and sediment yield: a global overview. Erosion and sediment yield: global and regional perspectives. Proc. Exeter Symp, July 1996. IAHS Publish, 1996, 236: 3~19.

[8] Schlesinger W H, Melack J M. Transport of organic carbon in the world's rivers. Tellus, 1981, 33(2): 172~187

[9] 方精云，刘国华，徐嵩龄. 中国陆地生态系统的碳循环及其全球意义. 见：王庚辰，温玉璞主编. 温室气体浓度和排放监测及相关过程.北京：中国环境科学出版社，1996，129~139

[10] Ritchie J C.Organic matter content in sediment of three navigation pools along the upper Mississippi River. Journal of Freshwater Ecology, 1988, 4: 343~349.

[11] Ritchie J C. Carbon content of sediments of small reservoirs. Water Resources Bulletin,1989, 25: 301~308.

[12] Lal R. World cropland soils as a source or sink for atmospheric C. Adv Agron 2000,71: 145~91.

[13] Lal R, Kimble J, Follett R. Knowledge gaps and researchable priorities. In: Lal R, Kimble J M, Follett R F, Stewart B A. (Eds.) Soil Processes and the Carbon Cycle. CRC Press, Boca Raton, FL, 1998, 595~604.

[14] Pennock D J, Anderson D W, de Jong E. Landscape-scale changes in indicators of soil quality due to cultivation in Saskatchewan. Canada. Geoderma, 1994, 64, 1~19.

[15] VandenBygaart A J. Erosion and deposition history derived by depth-stratigraphy of 137Cs and soil organic carbon. Soil & Tillage Research,2001,61: 187~192

[16] Ritchie J C, McCarty G W. 137Cesium and soil carbon in a small agricultural watershed. Soil & Tillage Research，2003，69 :45~51

[17] Stallard R F. Terrestrial sedimentation and the carbon cycle: coupling weathering and erosion to carbon burial. Global Biogeochem. Cycles , 1998,12: 231~257.

[18] Harden J W, Sharpe J M, Parton W P, Ojima D S, Fries T L, Huntington T G, Dabney S M. Dynamic replacement and loss of soil carbon on eroding cropland. Global Biogeochem. Cycles, 1999, 14 (4): 855~901.

[19] McCarty G W, Ritchie J C. Impact of soil movement on carbon sequestration in agricultural ecosystems. Environmental Pollution, 2002, 116: 423~430.

[20] Aerts R, Verhoeven J T A, Whigham D F. Plant-mediated controls on nutrient cycling in temperate fens and bogs. Ecology, 1999,80: 2170~2181.

[21] Bedford B L, Walbridge M R ， Aldous A. Patterns in nutrient availability and plant diversity of temperate North American wetlands. Ecology ，1999，80: 2151~2169.

[22] Gregorich E.G., Greer K.J. Anderson D W, Liang B C. Carbon distribution and losses: erosion and deposition effects .Soil & Tillage Research, 1998,47: 291~302

[23] Chen J S, Chiu C Y. Effect of topography on the composition of soil organic substances in a perhumid sub-stropical montane forest ecosysteminTaiwan. GEODERMA, 2000,96:19~30

[24] Gregorich E G. Soil quality: A Canadian perspective. In: Cameron K C, Cornforth I S , McLaren R G , Beare M H, Basher L R, Metherell A K, Kerr L E. (Eds.), Soil Quality Indicators for Sustainable Agriculture in New Zealand: Proceedings of a Workshop. Lincoln University, Christchurch, New Zealand, 1996，40~52.

[25] Schimel D S, Coleman D C, Horton K A. Soil organic matter dynamics in paired rangeland and cropland toposequences in North Dakota. Geoderma. 1985a, 36：201~214.

[26] Woods L E, Schuman G E. Cultivation and slope position effects on soil organic matter. Soil Sci. Soc. Am. J. 1988, 52:1371~1376.

[27] Schimel D S, Kelly E F, Yonker C, Aguilar R, Heil R. Effects of erosional processes on nutrient cycling in semiarid landscapes. In: Caldwell D E, Brierley J A, Brierley C L. (Eds.), Planetary Ecology. Van Nostrand Reinhold, New York, NY, 1985b, 571~580.

[28] Van Veen J A, Paul E A. Organic carbon dynamics in grassland soils. 1. Background information and computer simulation
[J]. Can. J. Soil Sci., 1981, 61:185~201.

[29] Paustian K. Use of a network of long-term experiments for analysis of soil carbon dynamics and global change: the North American model. Australian journal of experimental agriculture. 1995, 35 (7): 929~939.

[30] Batjes N H. Total carbon and nitrogen in the soils of the word. Eur .J . Soil .Sci ., 1996,47:151~163.

[31] Anderson D W . Decomposition of organic matter and carbon emissions from soils .in: Lal R et al(eds). Soil management and greenhouse effect. Advances in Soil Science .CRC Press Boca Raton .FL,165~175.

[32] Bajracharya R M, Lal R, Kimble J M. Diurnal and Seasonal CO2_C Flux from Soil as Related to Erosion Phases in Central Ohio
[J].Soil .Sci.Soc.Am .J. 2000, 64:286~293.

[33] Tisdall JM. Formation of soil aggregates and accumulation of soil organic matter. In: Carter MR, Stewart BA, editors. Structure and organic matter storage in agricultural soils. Boca Raton: CRC/Lewis Publishers; 1996, 57~96.

[34] Tisdall J M, Oades, J M.Organic matter and water stable aggregates in soils. J. Soil Sci. 1982,33:141~163.

[35] Benito E, Diza-Fierros F. Effect of cropping on the structural stability of soils rich in organic matter. Soil and Tillage Research, 1992,23:153~161.

[36] Boix-Fayos C, Calvo-Cases A, Imeson A C, et al., Influence of soil properties on the aggregation of some Mediterranean soils and the use of aggregate size and stability as land degradation indicators. Catena, 2001, 44: 47~67.

[37] Le bissonnais Y, Arrouays D. Aggregate stability and assessment of soil crustability and erodibility: II Application to humic loamy soils with various organic carbon contents. Europ. J. Soil Sci. 1997, 48:39~49.

[38] Amezketa E. Soil aggregate stability: a review. J. Sustainable Agriculture. 1999, 14:83~151.

[39] Wark K, Warner C F, Air pollution: Origion and control. I.E.P., New York ,1976, p 519.

[40] Rose N L. Inorganic fly-ash spherules as pollution tracers.Environ. Pollut, 1996, 91:245~252.

[41] Capp J P, Spencer J D. Fly ash utilization:A Summary of applications and technology. Information circular 8483. U.S. Department of Interior Bureau of Mines. Washington, DC, 1970.

[42] Jones R L, Olson K R. Fly Ash Use as a Time Marker in Sedimentation Studies. Soil Sci. Am. J. 1990, 54: 855~859.

[43] 方华军、杨学明、张晓平.农田土壤有机碳动态研究进展.土壤通报, 2003, 34(5): 389~393.

[44] Lefroy R D B, Blair G J, Strong W M. P.Changes in soil organic matter with cropping as measured by organic carbon fractions and 13C natural isotope abundence. Plant Soil. 1993.155/156:399~402.

[45] Bernoux M, Cerri C C, Neill C, et al. The use of stable carbon isotopes for estimating soil organic matter turnover rates . Geoderma 1998, 82:43~58.

[46] Collins H P, Elliott E T, Paustian K, et al. Soil carbon pools and fluxes in long-term corn belt agroecosystems. Soil Biology & Biochemistry. 2000,32:157~168.

[47] Roscoe R，Buurman P, Velthorst E J, et al. Soil organic matter dynamics in density and particle size fractions as revealed by the 13C/12C isotopic ratio in a Cerrado’s oxisol. GEODERMA. 2001, 104:185~202.

[48] 朴河春, 余登利. 林地变为玉米地后土壤轻质部分有机碳的13C/12C比值的变化. 土壤与环境, 2000, 9(3): 218~222.