土地利用变化与土壤地理

土壤粗有机质的研究进展

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  • 1. 中国科学院东北地理与农业生态研究所长春130012|2 加拿大农业部Harrow研究中心安大略, N0R 1G0|
    3. 中国科学院研究生院北京100039
梁爱珍( 1979- )| 女, 山西省交城县人, 博士研究生, 主要从事土壤管理和土壤有机质研究. E- mail: liang7973@yahoo.com.cn

收稿日期: 2005-12-01

  修回日期: 2006-04-01

  网络出版日期: 2006-05-25

基金资助

国家自然科学基金项目“黑土固定大气二氧化碳的潜力”(40271108)、国家自然科学基金项目“黑 土有机碳的时空分布特征与储量的关系”( 40471125) 和吉林省科技发展计划资助项目 ( 20050206- 4) 资助.

Review on Study of the Soil Macro- organic Matter

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  • 1. Northeast Institute of Geography and Agricultural Ecology, CAS, Changchun 130012, China|
    2. Harrow Research Centre, Agriculture &|Agri- Food Canada, Ontario, N0R 1G0, Canada|
    3. Graduate School of the Chinese Academy of Sciences, Beijing 100039, China

Received date: 2005-12-01

  Revised date: 2006-04-01

  Online published: 2006-05-25

摘要

土壤粗有机质是土壤中较为活跃的组分, 其密度组分对土壤有机质总矿化量有着重要贡 献, 可以作为评价管理措施转变引起土壤有机质短期变化的敏感性指标。分别介绍了按照不同的 物理分组方法划分的土壤有机质各物理组分的概念、土壤粗有机质及其分离方法, 探讨了影响土 壤粗有机质数量的主要因素( 管理措施、土地利用方式、土壤质地和气候条件) 和当前在研究土壤 粗有机质过程中存在的问题: ( 1) 各影响因素引起的土壤有机质变化的机制还不确定; ( 2) 土壤粗 有机质的分离方法还有待深入研究; ( 3) 粗有机质对土壤有机氮矿化的贡献认识还存在分歧。指 出探求更好的土壤粗有机质的分离方法和粗有机质对各影响因素的响应机制, 揭示土壤粗有机 质对土壤氮矿化的贡献是今后的主要研究方向。

本文引用格式

梁爱珍,张晓平,杨学明,方华军 . 土壤粗有机质的研究进展[J]. 地理科学进展, 2006 , 25(3) : 128 . DOI: 10.11820/dlkxjz.2006.03.015

Abstract

Soil macro- organic matter (MOM) with a rapid turnover rate plays a dominant role in soil nutrient dynamics, especially soil nitrogen. MOM is a significant component of light organic matter in soils. It can be a sensitive index to reflect the short- term effects of the management on soil organic matter. This paper reviews the concepts of various soil organic matter (SOM) fractions by different physical fractionations, details the fractionation methods for soil macro- organic matter (MOM), discusses the factors which have influences on the content of the soil MOM, factors which include management, land use, soil texture and climate. In the end, this paper points out the existing problems about the study of MOM: (1) The dynamic mechanism of soil organic matter is still puzzling. (2) The procedure for the separation of the soil MOMfraction needs to be studied further. (3)Many researchers'opinions diverge from each other on the contribution of MOM to soil nitrogen mineralization. In future, the study should focus on the mechanism of MOM responding to affecting factors, separating methods and the contribution of MOMto soil nitrogen mineralization.

参考文献


[1] Christensen B T. Physical fractionation of soil and organic matter in primary particle size and density separates . In: Stewart B A et al., eds. Advances in Soil Science. New York: Springer Verlag, 1992, 20: 2~90.

[2] Willson T C. Nitrogen Mineralization potential and macro organic matter: seasonal dynamics and cross- treatment. Available from: Kellogg Farm Report via the Internet Accessed 1997.

[3] Tiessen H and Stewart J W B. Particle- size fractions: II. Cultivation effects on organic matter composition in size fractions. Soil Science Society America Journal, 1983, 47: 509~514.

[4] Tiessen H and Stewart J W B and Hunt H W. Concepts of soil organic matter transformations in relation to organio- mineral particle size fractions. Plant and Soil, 1984, 76: 287~295.

[5] Dalal R C, Mayer R J. Long- term trends in fertility of soils under continuous cultivation and cereal cropping in southern Queensland. III. Distribution and kinetics of soil organic carbon in particle- size fractions. Australian journal of agricultural research, 1986, 24: 293~300.

[6] Hassink J. Density fractions of soil macro organic matter and microbial biomass as predictors of C and N mineralization. Soil Biology & Biochemistry, 1995, 27(8): 1099~1108.

[7] Ni J Z, Xu J M, Xie Z M. Soil light organic matter. Techniques and Equipment for Environmental Pollution, 2000, 1 ( 2) : 59~64.

[8] Wu J G, Zhang X Q, Wang Y H, et al. The effects of land use changes on the distribution of soil organic carbon in physical fractionation of soil. Forest Science, 2002, 38 (4): 19~29.

[9] Jennifer L Evans, Fernandez Ivan J, Lindsey E Rustad, et al. Methods for Evaluating Carbon Fractions in Forest Soils: A Review. Technical Bulletin 2001, 178: 12~18.

[10] Meijboom F W, Hassink J and Noordwijk M Van. Density fractionation of soil macroorganic matter using silica suspensions. Soil Biology & Biochemistry, 1995, 27(8): 1109~1111.

[11] Gregorich E G, and Janzen H H. Storage of soil carbon in the light fraction and macroorganic matter. In: Carter M R and Stewart B A eds. Structure and Organic Matter Agricultural Soils, Incorporation Boca Raton, Florida: CRC Press, 1996, 167~190.

[12] Hassink J. Preservation of plant residues in soils differing in unsaturated protective capacity. Soil Science Society America Journal, 1996, 60: 487~491.

[13] Magid J, Gorissen A and Giller K E. In search of the elusive ‘active'fraction of soil organic matter: Three size- density fractionation methods for tracing the fate of homogenously 14Clabeled plant materials. Soil Biology & Biochemistry, 1996,28: 89~99.

[14] Hassink J, Whitmore A P, andKubat J. Size and density fractionation of soil organic matter and the physical capacity of soils to protect organic matter. European Journal of Agronomy, 1997, 7: 189~199.

[15] Ellert B H, Gregorich E G. Management - induced changes in the actively cycling fractions of soil organic matter . In McFee W W and Kelly J M eds. Carbon Forms and functions in Forest Soils. Incorporation, Madison, Wisconsin: Soil Science Society America Journal, 1995, 119~138.

[16] Monaghan R and Brraclough D. Contributions to N mineralization from soil macroorganic matter fractions incorporated into two field soils. Soil Biology & Biochemistry, 1997, 29( 8) : 1215~1223.

[17] Yakovchenko V P, Sikora L J and Miliner P D. Carbon and nitrogen mineralization of added particulate and macroorganic matter. Soil Biology & Biochemistry, 1998, 30 (14): 2139~2146.

[18] Warren G P, Whitehead D C. Available soil nitrogen in relation to fractions of soil nitrogen and other soil properties. Plant and Soil, 1988, 112: 155~165.

[19] Craft C B, Broome S W and Seneca E D. Nitrogen, phosphorus and organic carbon pools in natural and transplanted marsh soils. Estuaries, 1988, 11:272~280.

[20] Monaghan R, Brraclough D. Contributions to gross N mineralization from 15N- labelled soil macroorganic matter frations during laboratory incubation. Soil Biology & Biochemistry, 1996, 27(12): 1623~1628.

[21] Willson T C, Paul E A, Harwood R R. Biologically active soil organic matter fraction in sustainable cropping systems. Applied Soil Ecology, 2000, 16: 63~76.

[22] Plewinsky B. and Kamps R. Sodium metatungstate, a new medium for binary and ternary density gradient centrifugation. Makromolare Chemie . 1984, 185: 1429~1439.

[23] Cambardella C A, Elliott E T. Carbon and nitrogen dynamics of soil organic matter fractions from cultivated grassland soils. Soil Science Society America Journal, 1994, 58: 123±130.

[24] Six J, Schultz P A, Jastrow J D, et al.. Recycling of sodium polytungstate used in soil organic matter. Soil Biology & Biochemistry, 1999, 31: 1193~1196.

[25] 黄昌勇. 土壤学. 北京: 中国农业出版社, 1999.

[26] Gerzabek M H, Haberhauer G, Kirchman H. Soil organic matter pools and carbon 13 natural abundance in particle size fractions of a long term agricultural field experiment receiving organic amendments. Soil Science Society America Journal, 2001, 65 (2): 352 ~ 358.

[27] Alessandra A Freixoa, Pedro Luiz O de A Machadob, Henrique P dos Santosc, et al.. Soil organic carbon and fractions of a Rhodic Ferralsol under the influence of tillage and crop rotation systems in southern Brazil. Soil & Tillage Research, 2002, 64: 221~230.

[28] Raupp Joachim, Oltmanns Meike. Fractions of particulate organic matter in soils depending upon farmyard manure and mineral fertilization . In: Proceedings of the 14th IFOAMOrganic World Congress, 2002, 25.

[29] Johansson G. Production and turnover of roots and root derived organic C
[Dissertation]. Upsala: Swedish University of Agricultural Sciences, 1994.

[30] Haynes R J, Beare M H. Structure and Organic Matter Storage in Agricultural Soils . In: Carter M R and Stewart B A eds. Advances in Soil Science. Boca Raton: CRC Lewis Publishers, 1996, 213~262.

[31] Barrios E, Buresh R J, Sprent J I. Organic matter in soil particle size and density fractions from maize and legume cropping systems. Soil Biology & Biochemistry, 1996, 28: 185~193.

[32] Guggenberger G, Zech W, Thomas R J. Lignin and carbohydrate alteration in particle size separates of an Oxisol under tropical pasture following native grassland. Soil Biology & Biochemistry, 1995, 27: 1629~1638.

[33] Silva C A, Anderson S J, Vale F R. Effect of long- term cultivation on soil organic matter quality in some agricultural systems in the Brazilian Cerrado region . In: 88th Annual Meeting of the American Society of Agronomy. Indianapolis, Globalization: a challenge for change, 1996.

[34] Hassink J. Relationship between the amount and the activity of the microbial biomass in Dutch grassland soils: comparison of the fumigation- incubation method and the substrate- induced respiration method. Soil Biology & Biochemistry, 1993, 25: 533~538.

[35] Zech W, Haumaier L, Kogel- Knabner I. Changes in aromaticity and carbon distribution of soil organic matter due to pedogenesis. The Science of the Total Environment, 1989, 81r 82: 179~186.

[36] Schimel D S, Braswell B H, Holland E A, et al. Climatic, edaphic and biotic controls over storage and turnover of carbon in soils. Global Biogeochemical Cycles, 1994, 8: 279~293.

[37] Trumbore S E, Chadwick O A, Amundson R. Rapid exchange of soil carbon and atmospheric CO driven by temperature change. Science, 1996, 272: 393~396.

[38] Chan K Y, Heenan D P, Oates A. Soil carbon fractions and relationship to soil quality under different tillage and stubble management. Soil & Tillage Research, 2002, 63: 133~139.

[39] Angers Denis A. Water- stable aggregation of Québec silty clay soils: some factors controlling its dynamics. Soil & Tillage Research, 1998, 47: 91~96.

[40] Carter M R, Angers D A, Gregorich E. G., and Bolinder M. A.. Characterizing organic matter retention for surface soils in eastern Canada using density and particle size fractions. Canadian Journal of Soil Science, 2003, 83( 1) : 11~23.

[41] Adams T M. Macroorganic matter content of some Northern Ireland soils. Northern Ireland Record of Agricultural Research, 1980, 28: 1~12.

[42] Christensen B T. Decomposability of organic matter in particle size fractions from field soils with straw incorporation. Soil Biology & Biochemistry, 1987, 33: 365~373.

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