有机物料还田对麦玉两熟农田土壤有机碳和系统碳净平衡影响研究
详细信息    本馆镜像全文|  推荐本文 |  |   获取CNKI官网全文
摘要
针对我国农业废弃物类多、数量大、利用低、污染重的现实问题,以循环农业理念为指导,选择代表农田内循环的秸秆、代表农牧循环的猪粪、代表农沼循环的沼渣、代表农菌循环的菌渣、代表农工循环的酒渣5种有机物料进行等碳量还田,通过麦玉两熟农田定位试验,重点对土壤有机碳及其组分变化、团聚体固碳机制、土壤温室气体排放进行监测与分析,研究不同物料还田对农田系统的碳平衡的影响及其机制。试验开始于2010年6月,本论文主要分析2012-2013年的数据。取得的主要进展主要有:
     (1)五种物料还田均能不同程度促进麦玉两熟集约化农田土壤总有机碳积累,增强系统固碳潜力。与单施无机肥相比,5种物料还田3年后的土壤有机碳(TOC)含量平均提高44%,周年系统固碳量分别增加4.22~6.30t C ha-1。与不施肥(NF)和撂荒地(FL)相比,物料还田的TOC含量分别高出63%和32%,系统固碳量平均增加8.78t C ha-1和6.82t C ha-1。综合表明,循环农作模式对土壤TOC积累正贡献最大,非循环农作模式(无机肥)与原始农作模式(不施肥)对TOC积累呈现负贡献,撂荒模式TOC相对稳定。
     (2)五种物料中,猪粪、沼渣和菌渣更有利于土壤有机碳的积累和系统固碳潜力的提高。猪粪、沼渣、菌渣和酒渣的TOC含量分别比秸秆处理高29%、27%、27%和16%,表明经过其他系统“循环”利用的有机物还田比秸秆直接还田更有利于有机碳在土壤中积累。猪粪、沼渣和菌渣还田3年后分别比秸秆直接还田多积累1.26tCha-1,0.76tCha-1,0.26tCha-1。
     (3)有机物料还田促进土壤团聚体的形成,有利于对土壤有机碳的保护,其中猪粪、沼渣和菌渣大幅提高有机碳的稳定性。有机物料还田的微团聚体结合态TOC以及大团聚体包裹的微团聚体结合态TOC含量分别比撂荒、非循环农作模式及原始农作模式高54%,115%,128%。菌渣、猪粪、沼渣和酒渣还田的土壤微团聚体结合态TOC以及大团聚体包裹的微团聚体结合态TOC含量分别比秸秆高49%、23%、22%和7%,说明经过农田系统外循环回来的物料还田有利于TOC稳定性的提高。
     (4)有机物料还田虽促进了土壤温室气体排放,但同时也提高了系统碳输入,最终表现出系统固碳能力增强,是温室气体的“汇”。五种物料还田的土壤温室气体排放增温潜势平均比无机肥高出58%,但同时也提高了系统生产力、增加系统固碳,弥补所促进的温室气体排放量,从而使整个系统的表现为碳汇,系统净碳平衡高出264%。
     研究结果表明,农田有机废弃物经过农牧循环、农沼循环、农菌循环之后回田,具有更强的固碳优势,又能提高系统生产力,说明发展循环农业,促进农业节能减排具有重要意义。
A large number of agricultural organic wastes are produced in China every year from various agricultural systems. The low utilization of these organic wastes leads to serious potential pollution to the environment. To resolve these problems, five types of organic wastes were applied to a wheat-maize cropping system based on the concept of circular agriculture, including crop straw (CS) representing the inner farmland circulation, pig manure (PM) representing the farming-stockbreeding circulation, biogas residue (BR) representing the farming-biogas circulation, mushroom residue (MR) representing the farming-mushroom circulation, and wine residue (WR) representing farming-processing circulation. The organic wastes were incorporated at an equal rate of carbon. Total organic carbon (TOC) and its components, soil aggregate, and soil greenhouse gases (GHGs) emission were investigated and analyzed to explore the effects of organic waste on soil organic carbon and net carbon balance of the farming system. This experiment began in June2012, data in the period of2012to2013were analyzed in this dissertation. The main results were as follows.
     (1) Incorporation of the five organic wastes could promote the accumulation of TOC in the wheat-maize intensive farming system, and improve the retention of C in the system. In comparison with CF, TOC was increased by44%on average after three years of organic waste incorporation, the amount of C retention in the system increased4.22-6.30t C ha-1. When compared with the no-fertilization (NF) and fallow (FL), TOC were increased by63%and32%, respectively, and the amount of C retention were increased8.78t C ha-1and6.82t C ha-1. On the whole, the largest positive contribution to the accumulation of TOC was derived from the circular farming mode, and the negative contribution were showed in the acyclic farming mode (CF) and primeval farming mode (NF), whereas a stable TOC was showed in the fallow mode.
     (2) Among the five orgaic wastes, pig manure, biogas residue and mushroom residue are more benefit to the accumulation of TOC and improvement of C retention. In comparison with CS, the TOC of PM, BR and WR were increased by29%,27%,27%and16%respectively, which indicated that it was more conducive to soil C accumulation by incorporating organic wastes recycling from other systems than crop straw. The amount of C retention in the system raised by1.26tC ha-1,0.761C ha-1,0.261C ha-1in PM, BR and MR when compared to CS.
     (3) Incorporating organic wastes promotes the formation of soil aggregate, and is beneficial for the protection of TOC, among the organic wastes, PM, BR and MR greatly increase the stability of soil organic C. In comparison with FL, CF and NF, the microaggregate associated TOC and microaggregate-within-macroaggregate associated TOC content were increased by54%,115%and128%in organic wastes treatments. The microaggregate associated TOC and microaggregate-within-macroaggregate associated TOC contents in MR, PM, BR and WR were49%,23%,22%and7%higher than that of CS, which indicated that the returning back of organic wastes from the outside systems were more conducive to the improvement of the TOC stability.
     (4) Although organic wastes incorporation promote GHGs emissions, it also increases carbon input of farming system, and ultimately presents an enhancement in C retention capacity of the system which served as greenhouse gases "sinks". The soil greenhouse gas warming potential (GWP) of the five organic waste treatments was58%higher than CF, the fact that the net primary production (NPP), system C retention were also improved, could easily offset the promoted GHG emissions, so that the whole system turned out a sink of C, and the net carbon balance (NECB) was increased by264%.
     The results showed that advantages of C retention and system production can derive from the returning back of organic wastes from the farming-stockbreeding circulation system, the farming-biogas circulation system and the farming-mushroom circulation system. This indicated that it is of great importance to develop circular agriculture, to promote the energy-saving and emissions reduction.
引文
[1]Abiven S, Menasseri S, Chenu C. The effects of organic inputs over time on soil aggregate stability-Aliterature analysis. Soil Biology and Biochemistry,2009,41:1-12.
    [2]Agbenin J O, Goladi J T. Carbon, nitrogen and phosphorus dynamics under continuous cultivation as influenced by farmyard manure and inorganic fertilizers in the savanna of northern Nigeria. Agriculture, Ecosystems and Environment,1997,63:17-24.
    [3]Amelung W, Zhang X, Flach K W, et al. Amino sugars in native grassland soils along a climosequence in North America. Soil Science Society of America Journal,1999,63:86-92.
    [4]Angers D A, Recous S, Aita C. Fate of carbon and nitrogen in water-stable aggregates during decomposition of 13C15N-labelled wheat straw in situ. European Journal of Soil Science,1997, 48:295-300.
    [5]Aoyama M, Angers D A, N'Dayegamiye A, et al. Protected organic matter in water-stable aggregates as affected by mineral fertilizer and manure applications. Canadian Journal of Soil Science,1999,79:419-425.
    [6]Aoyama M, Angers D A, N'Dayegamiye A, et al. Metabolism of 13C-labeled glucose in aggregates from soils with manure application. Soil Biology & Biochemistry,2000,32:295-300.
    [7]Ashman M R, Hallett P D, Brookes P C. Are the links between soil aggregate size class, soil organic matter and respiration rate artefacts of the fractionation procedure. Soil Biology and Biochemistry, 2003,35:435-444.
    [8]Baggs E M, Rees R M, Smith K A, et al. Nitrous oxide emission from soils after incorporating crop residues. Soil Use Manage,2000,16:82-87.
    [9]Baldock J A, Masiello C A, Gelinas Y, et al. Cycling and composition of organic matter in terrestrial and marine ecosystems. Marine Chemistry,2004,92:39-64.
    [10]Ball B C, Scott A, Parker J P. Field N2O, CO2 and CH4 fluxes in relation to tillage, compaction and soil quality in Scotland. Soil & Tillage Research,1999,53:29-39.
    [11]Beare M H, Hendrix P F, Coleman D C. Water-stable aggregates and organic matter fractions in conventional and no-tillage soils. Soil Science Society of American Journal,1994,58:777-786.
    [12]Berg B. Nutrient release from litter and humus in coniferous forest soils-a mini review. Scandinavian Journal of Forest Research,1986,1:359-369.
    [13]Berg B, Matzner E. Effect of N deposition on decomposition of plant litter and soil organic matter in forest systems. Environmental Reviews,1997,5:1-25.
    [14]Bhattacharyya R, Kundu S, Srivastva A K, et al. Long term fertilization effects on soil organic carbon pools in a sandy loam soil of the Indian sub-Himalayas. Plant Soil,2011,341:109-124.
    [15]Bingeman C W, Varner J, Martin W. The effect of the addition of organicmaterials on the decomposition of an organic soil. Soil Science Society of America Journal,1953,17:34-38.
    [16]Blagodatskaya E, Kuzyakov Y. Mechanisms of real and apparent priming effects and their dependence on soil microbial biomass and community structure:critical review. Biology and Fertility of Soils,2008,45:115-31.
    [17]Blair G J, Lefroy R D B, Lisle L. Soil carbon fractions based on their degree of oxidation, and the development of a carbon management index for agricultural systems. Australian Journal of Agricultural Research,1995,46:1459-1466.
    [18]Blanchette R A. Delignification by wood-decay fungi. Annual Review of Phytopathology,1991, 29:381-398.
    [19]Bol R, Kandeler E, Amelung W, et al. Short-term effects of dairy slurry amendment on carbon sequestration and enzyme activities in a temperate grassland. Soil Biology and Biochemistry,2003, 35:1411-1421.
    [20]Bossuyt H, Denef K, Six J, et al. Influence of microbial populations and residue quality on aggregate stability. Applied Soil Ecology,2001,16:195-208.
    [21]Briedis C, Moraes Sa J C, Caires E F, et al. Soil organic matter pools and carbon-protection mechanisms in aggregate classes influenced by surface liming in a no-till system. Geoderma,2012, 170:80-88.
    [22]Cao M, Woodward F I. Net primary and ecosystem production and carbon stocks of terrestrial ecosystems and their responses to climate change. Global Change Biology,1998,4:185-198.
    [23]Carter M R. Soil quality for sustainable land management. Agronomy Journal,2002,94:38-47.
    [24]Cayuela M L, Velthof G L, Mondini C, et al. Nitrous oxide and carbon dioxide emissions during initial decomposition of animal by-products applied as fertilisers to soils. Geoderma,2010, 157:235-242.
    [25]Chaves B, De Neve S, Cabrera M C, et al. The effect of mixing organic biological waste materials on high-N crop residues on the short time N2O emission from horticultural soil in model experiments. Biology and Fertility of Soils,2005,41:411-418.
    [26]Chirinda N, Olesen J E, Porter J R, et al. Soil properties, crop production and greenhouse gas emissions from organic and inorganic fertilizer-based arable cropping systems. Agriculture, Ecosystems and Environment,2010,139:584-594.
    [27]Chivenge P, Vanlauwe B, Gentile R, et al. Organic and Mineral Input Management to Enhance Crop Productivity in Central Kenya. Agronomy Journal,2009,101:1266-1275.
    [28]Chivenge P, Vanlauwe B, Gentile R, et al. Organic resource quality influences short-term aggregate dynamics and soil organic carbon and nitrogen accumulation. Soil Biology and Biochemistry, 2011a,43:657-666.
    [29]Chivenge P, Vanlauwe B, Gentile R, et al. Comparison of organic versus mineral resource effects on short-term aggregate carbon and nitrogen dynamics in a sandy soil versus a fine textured soil. Agriculture, Ecosystems and Environment,2011b,140:361-371.
    [30]Christensen B T, Johnston A E. Soil organic matter and soil quality-lessons learned from long-term field experiments at Askov and Rothamsted. In:Gregorich, E.G., Carter, M.R. (Eds.), Soil Quality for Crop Production. Soil Quality for Crop Production and Ecosystem Health. Developments in Soil Science, Vol.25. Elsevier, Amsterdam,1997, pp.399-430.
    [31]Christensen B T. Physical fractionation of soil and organic matter in primary particle size and density separates. Advances in soil science,1992,20:1-89.
    [32]Chung H, Ngo K J, Plante A F, et al. Evidence for carbon saturation in a highly structured and organic-matter-rich soil. Soil Science Society of American Journal,2010,74:130-138.
    [33]Denef K, Zotarelli L, Boddey R M, et al. Microaggregate-associated carbon as a diagnostic fraction for management-induced changes in soil organic carbon in two Oxisols. Soil Biology and Biochemistry,2007,39:1165-1172.
    [34]Dubey A, Lal R. Carbon footprint and sustainability of agricultural production systems in Punjab, India, and Ohio, USA. Journal of crop improvement,2009,23:332-350.
    [35]Duiker S W, Rhoton F E, Torrent J, et al. Iron (hydr)oxide crystallinity effects on soil aggregation. Soil Science Society of America Journal,2003,67:606-611.
    [36]Duiker S W, Lal R. Crop residue and tillage effects on carbon sequestration in a Luvisol in central Ohio. Soil and Tillage Research,1999,52:73-81.
    [37]Elliott E T. Aggregate structure and carbon, nitrogen, and phosphorus in native and cultivated soils. Soil Science Society of American Journal,1986,50:627-633.
    [38]Elliott E T, Coleman D C. Let the soil work for us. Ecological Bulletins,1988,39:23-32.
    [39]Elson J. A comparison of the effect of fertilizer and manure, organic matter, and carbon-nitrogen ratio on water-stable soil aggregates. Soil Science Society of American Journal,1942,6:86-90.
    [40]Elson J. A 4-year study of the effects of crop, lime, manure, and fertilizer on macroaggregation of dunmore silt loam. Soil Science Society of American Journal,1944,8:87-90.
    [41]Enriquez S, Duarte C M, Sand-Jensen K. Patterns in decomposition rates among photosynthetic organisms:the importance of detritus C:N:P content. Oecologia,1993,94:457-471.
    [42]Feller C, Beare M H. Physical control of soil organicmatter dynamics in the tropics. Geoderma, 1997,79:69-116.
    [43]Feng K, Wang X L, Wang X Z. Relationship between 2:1 mineral structure and the fixation and release of cations. Pedosphere,2003,13(1):81-86.
    [44]Firestone M K, Davidson E A. Microbiological basis for NO and N2O production and consumption in soils. In:Andreae M, Schimel ODS (eds) Exchange of trace gases between terrestrial ecosystems and the atmosphere. Wiley, New York,1989. pp7-21.
    [45]Fog K. The effect of added nitrogen on the rate of decomposition of organic matter. Biological Reviews of the Cambridge Philosophical Society,1988,63:433-462.
    [46]Fontaine S, Mariotti A, Abbadie L. The priming effec t of organic matter:A ques t i on of microbial competition? Soil Biology and Biochemistry,2003,35:837-843.
    [47]Fonte S J, Quansah E Y P O G W, Vanlauwe B, et al. Fertilizer and residue quality effects on organic matter stabilization in soil aggregates. Soil Science Society of American Journal,2009, 73:961-966.
    [48]Gentile R, Vanlauwe B, Six J. Litter quality impacts short-but not long-term soil carbon dynamics in soil aggregate fractions. Ecological Applications,2011,21:695-703.
    [49]Gentile R, Vanlauwe B, Chivenge P, et al. Interactive effects from combining fertilizer and organic residue inputs on nitrogen transformations. Soil Biology and Biochemistry,2008,40:2375-2384.
    [50]Gentile R, Vanlauwe B, Kavoo A, et al. Residue quality and N fertilizer do not influence aggregate stabilization of C and N in two tropical soils with contrasting texture. Nutrient Cycling in Agroecosystems,2010,88:121-131.
    [51]Gentile R, Vanlauwe B, Kessel C, et al. Managing N availability and losses by combining fertilizer-N with different quality residues in Kenya. Agriculture, Ecosystems & Environment, 2009,131:308-314.
    [52]Ginting D, Kessavalou A, Eghball B, et al. Greenhouse gas emissions and soil indicators four years after manure and compost applications. Journal of Environmental Quality,2003,32:23-32.
    [53]Granli T, B(?)ckman O C. Nitrous oxide from agriculture. Norwegian Journal of Agricultural Science 12 (Suppl),1994,1-128.
    [54]Gregorich E G, Rochette P, VandenBygaart A J, et al. Greenhouse gas contributions of agricultural soils and potential mitigation practices in Eastern Canada. Soil and Tillage Research,2005, 83:53-72.
    [55]Gregory P J. Roots, rhizosphere and soil:the route to a better understanding of soil science? European Journal of Soil Science,2006,57:2-12.
    [56]Gong W, Yan X Y, Wang J Y, et al. Long-term manuring and fertilization effects on soil organic carbon pools under a wheat-maize cropping system in North China Plain. Plant Soil,2009, 314:67-76.
    [57]Guggenberger G, Christensen B T, Zech W. Land-use effects on the composition of organic matter in particle-size separates of soils:I. Lignin and carbohydrate signature. European Journal of Soil Science,1994,45:449-458.
    [58]Glude S, Chung H, Amelung W, et al. Soil carbon saturation controls labile and stable carbon pool dynamics. Soil Science Society of American Journal,2008,72:605-612.
    [59]Hadas A, Kautskya L, Goekb M, et al. Rates of decomposition of plant residues and available nitrogen in soil, related to residue composition through simulation of carbon and nitrogen turnover. Soil Biology and Biochemistry,2004,36:255-266.
    [60]Haynes R J, Beare M H. Influence of six crop species on aggregate stability and some labile organic matter fractions. Soil Biology and Biochemistry,1997,29:1647-1653.
    [61]Hanson P J, Edwards N T, Garten C T, et al. Separating root and soil microbial contributions to soil respiration:a review of methods and observations. Biogeochemistry,2000,48:115-146.
    [62]Hassink J. Density fractions of soil macroorganic matter and microbial biomass as predictors of C and N mineralization. Soil Biology and Biochemistry,1995,27:1099-1108.
    [63]Hassink J. Preservation of plant residues in soil differing in unsaturated protect capacity. Soil Science Society of America Journal,1996,60:487-491.
    [64]Hassink J. The capacity of soils to preserve organic C and N by their association with clay and silt particles. Plant and Soil,1997,191:77-87.
    [65]Heal O W, Anderson J M, Swift J. Plant litter quality and decomposition:an historical overview. In: G. Cadisch and K. E. Giller, (eds). Driven by nature:plant litter quality and decomposition. CAB International, Wallingford, UK,1997, pp.3-30.
    [66]Henriksen T M, Breland T A. Nitrogen availability effects on carbon mineralization, fungal and bacterial growth, and enzyme activities during decomposition of wheat straw in soil. Soil Biology and Biochemistry,1999,31:1121-1134.
    [67]Howard D M, Howard P J A. Relationships between CO2 evolution, moisture content and temperature for a range of soil types. Soil Biology and Biochemistry,1993,25:1537-1546.
    [68]Huang J X, Chen Y Q, Sui P, et al. Estimation of net greenhouse gas balance using crop-and soil-based approaches:Two case studies. Science of the Total Environment,2013, 4456-457:299-306.
    [69]Huang Y, Zou J W, Zheng X H, et al. Nitrous oxide emissions as influenced by amendment of plant residues with different C:N ratios. Soil Biology and Biochemistry,2004,36:973-981.
    [70]IPCC. IPCC Fourth Assessment Report:Climate Change 2007, Charpter 4. http://www.ipcc.ch/publications_and_data/ar4/syr/zh/main.html
    [71]Jacobson M Z. Review of solutions to global warming, air pollution, and energy security. Energy and Environmental Science,2009,2:148-173.
    [72]Jager N, Stange C F, Ludwig B, et al. Emission rates of N2Oand CO2 from soils with different organic matter content from three long-term fertilization experiments. Biology and Fertility of Soils,2011,47:483-494.
    [73]Janzen H H. Soil organic matter characteristics after long-term cropping to various spring wheat rotations. Canadian Journal of Soil Science,1987,67:845-856.
    [74]Jastrow J D. Soil aggregate formation and the accrual of particulate and mineral associated organic matter. Soil Sciences Society of American Journal,1996,60:801-807.
    [75]Jastrow J D, Miller R M, Lussenhop J. Contributions of interacting biological mechanisms to soil aggregate stabilization in restored prairie. Soil Biology and Biochemistry,1998,30:905-916.
    [76]Jia J X, Ma Y C, Xiong Z Q. Net ecosystem carbon budget, net global warming potential and greenhouse gas intensity in intensive vegetable ecosystems in China. Agriculture, Ecosystems and Environment,2012,150:27-37.
    [77]Johnston A E. Soil organic carbon:effects on soils and crops. Soil Use Manage,1986,2:97-105
    [78]Johnson J M F, Franzluebbers A J, Weyers S L, et al. Agricultural opportunities to mitigate greenhouse gas emissions. Environmental Pollution,2007,150:107-124.
    [79]Kaiser K, Guggenberger G. Distribution of hydrous aluminium and iron over density fractions depends on organic matter load and ultrasonic dispersion. Geoderma,2007,140:140-146.
    [80]Karami A, Homaee M, Afzalinia S, et al. Organic resource management:Impacts on soil aggregate stability and other soil physico-chemical properties. Agriculture, Ecosystems and Environment, 2012,148:22-28.
    [81]Kemmitt S J, Lanyonb C V, Waite I S, et al. Mineralization of native soil organic matter is not regulated by the size, activity or composition of the soil microbial biomass-a new perspective. Soil Biology and Biochemistry,2008,40:61-73.
    [82]Kemper W D, Rosenau R C. Aggregate stability and size distribution. In Klute A, ed. Methods of soil analysis. Part 1.2nd ed. ASA and SSSA, Madison, WI,1986, pp.425-442.
    [83]Kiem R, Kogel-Knabner I. Contribution of lignin and polysaccharides to the refractory carbon pool in C-depleted arable soils. Soil Biology and Biochemistry,2003,35:101-118.
    [84]Knicker H. Stabilization of N-compounds in soil and organic-matter-rich sediments-what is the difference? Marine Chemistry,2004,92:167-195.
    [85]Kogel-Knabner I. The macromolecular organic composition of plant and microbial residues as inputs to soil organic matter. Soil Biology and Biochemistry,2002,34:139-162.
    [86]Korschens M. Relations between the share of fine particles, Ct and Nt contents in the soil. Archiv fur Acker-und Pflanzenbau und Bodenkunde,1980,24(9):585-592.
    [87]Korschens M, Weigel A, Schulz E. Turnover of soil organic matter (SOM) and long-term balances- tools for evaluating sustainable productivity of soils. Journal of Plant Nutrition and Soil Science, 1998,161:409-424.
    [88]Knops J M H,Tilman D. Dynamics of soil nitrogen and carbon accumulation for 61 years after agricultural abandonment. Ecology,2000,81:88-98.
    [89]Kong A Y Y, Six J, Bryant D C, et al. The Relationship between carbon Input, aggregation, and soil organic carbon stabilization in sustainable cropping systems. Soil Science Society of American Journal,2005,69:1078-1085.
    [90]Krull E S, Baldock J A, Skjemstad J O. Importance of mechanisms and processes of the stabilisation of soil organic matter for modelling carbon turnover. Functional Plant Biology,2003, 30:207-222.
    [91]Lal R. Soil Carbon sequestration impacts on global climatic change and food security. Science, 2004,304:1623-1627.
    [92]Lal R. Soil management and restoration for C sequestration to mitigate the accelerated greenhouse effect. Progress in Environmental Science,1999,1:307-326.
    [93]Lal R. Sequestering carbon in soils of agro-ecosystems. Food Policy,2011,36:33-39.
    [94]Lee C H, Park K D, Jung K Y, et al. Effect of Chinese milk vetch (Astragalus sinicus L.) as a green manure on rice productivity and methane emission in paddy soil. Agriculture, Ecosystems and Environment,2010,138:343-347.
    [95]Lin Q, Brookes P C. An evaluation of the substrate-induced respiration method. Soil Biology and Biochemistry,1999,31:1969-1983.
    [96]Liu E, Yan C, Mei X, et al. Long-term effect of chemical fertilizer, straw, and manure on soil chemical and biological properties in northwest China. Geoderma,2010,158:173-180.
    [97]Lorenz K, Lal R, Shipitalo M J. Stabilization of organic carbon in chemically separated pools in no-till and meadow soils in Northern Appalachia. Geoderma,2006,137:205-211.
    [98]Lou Y L, Xu M G, Wang W, et al. Return rate of straw residue affects soil organic C sequestration by chemical fertilization. Soil and Tillage Research,2011,113:70-73.
    [99]Lutzow M v, Kogel-Knabner I, Ekschmitt K, et al. Stabilization of organic matter in temperate soils:mechanisms and their relevance under different soil conditions - a review. European Journal of Soil Science,2006,57:426-445.
    [100]Mafongoya P L, Giller K E, Palm C A. Decomposition and nitrogen release patterns of tree prunings and litter. Agroforestry Systems,1997,38:77-97.
    [101]Magill A H, Aber J D. Long-term effects of experimental nitrogen additions on foliar litter decay and humus formation in forest ecosystems. Plant and Soil,1998,203:301-311
    [102]Maljanen M, Liikanen A, Silvola J, et al. Nitrous oxide emissions from boreal organic soil under different land-use. Soil Biology and Biochemistry,2003,35:689-700.
    [103]Mandal B, Majumder B, Adhya T K,et al. The potential of double-cropped rice ecology to conserve organic carbon under subtropical climate. Global Change Biology,2008,14:2139-2151.
    [104]Manna M C, Swarup A, Wanjari R H, et al. Long-term effect of fertilizer and manure application on soil organic carbon storage, soil quality and yield sustainability under sub-humid and semi-arid tropical India. Field Crops Research,2005,93:264-280.
    [105]Marseille F, Disnar J R, Guillet B, et al. n-Alkanes and free fatty acids in humus and A1 horizons of soils under beech, spruce and grass in the Massif-Central (Mont-Lozere), France. European Journal of Soil Science,1999,50:433-441.
    [106]Martens D A, Frankenberger W T. Modification of infiltration rates in an organic-amended irrigated. Agronomy Journal,1992,84:707-717.
    [107]Martens D A. Management and crop residue influence soil aggregate stability. Journal of Environmental Quality,2000a,29:723-727.
    [108]Martens D A. Plant residue biochemistry regulates soil carbon cycling and carbon sequestration. Soil Biology and Biochemistry,2000b,32:361-369.
    [109]Melillo J M, Aber J D, Muratore J F. Nitrogen and lignin control of hardwood litter decomposition dynamics. Ecology,1982,63:621-626.
    [110]Meng L, Ding W X, Cai Z C. Long-term application of organic manure and nitrogen fertilizer on N2O emissions, soil quality and crop production in a sandy loam soil. Soil Biology and Biochemistry,2005,37:2037-2045.
    [111]Monteith J L, Szeicz G, Yabuki K. Crop photosynthesis and the flux of carbon dioxide below the canopy. Journal of Applied Ecology,1964,1:321-337.
    [112]Mosier A R, Halvorson A D, Reule C A, et al. Net global warming potential and greenhouse gas intensity in irrigated cropping systems in northeastern Colorado. Journal of Environmental Quality, 2006,35:1584-1598.
    [113]Muller T, Hoper H. Soil organic matter turnover as a function of the soil clay content: consequences for model applications. Soil Biology and Biochemistry,2004,36:877-888.
    [114]Nichols J D. Relation of Organic Carbon to Soil Properties and Climate in the Southern Great Plains. Soil Science Society of America Journal,1984,48:1382-1384.
    [115]Oades J M. Soil organic matter and structural stability:mechanisms and implications for management. Plant Soil,1984,76:319-337.
    [116]Oades J M. The retention of organic matter in soils. Biogeochemistry,1988,5:35-70.
    [117]Oades J M, Waters A G. Aggregate hierarchy in soils. Australian Journal of Soil Research,1991, 29:815-828.
    [118]Osher L J, Matson P A, Amundson R. Effect of land use change on soil carbon in Hawaii. Biogeochemistry,2003,65:213-232.
    [119]Palm C A, Gachengo C N, Delve R J, et al. Organic inputs for soil fertility management in tropical agroecosystems:application of an organic resource database. Agriculture, Ecosystems and Environment,2001,83:27-42.
    [120]Palm C A, Rowland A P. A minimum dataset for characterization of plant quality for decomposition. Driven by nature:plant litter quality and decomposition. CAB Inter-national, Wallingford, UK.1997:379-392
    [121]Pan G X, Smith P, Pan W N. The role of soil organic matte in maintaining the productivity and yield stability of cereals in China. Agriculture, Ecosystems and Environment,2009,129:344-348.
    [122]Parton W, Silver W L, Burke I C, et al. Global-scale similarities in nitrogen release patterns during long-term decomposition. Science,2007,315:361-364.
    [123]Paustian K, Andren O, Janzen H H, et al. Agricultural soils as a sink to mitigate CO2 emissions. Soil use and Management,1997,13:230-244.
    [124]Plante A F, McGill W B. Soil aggregate dynamics and the retention of organic matter in laboratory-incubated soil with differing simulated tillage frequencies. Soil and Tillage Research, 2002,66:79-92.
    [125]Powlson D S, Bhogal A, Chambers B J. The potential to increase soil carbon stocks through reduced tillage or organic material additions in England and Wales:A case study. Agriculture, Ecosystems and Environment,2012,146:23-33.
    [126]Puget P, Chenu C, Balesdent J. Total and young organic matter distributions in aggregates of silty cultivated soils. European Journal of Soil science,1995,46:449-459.
    [127]Puget P, Drinkwater L E. Short-term dynamics of root-and shoot-derived carbon from a leguminous green manure. Soil Science Society of American Journal,2001,65:771-779.
    [128]Puttaso A, Vityakon P, Rasche F, et al. Does organic residue quality influence carbon retention in a tropical sandy soil? Soil Science Society of American Journal,2013,77:1001-1011.
    [129]Raich J W, Tufekcioglu A. Vegetation and soil respiration:correlations and controls. Biogeochemistry,2000,48:71-90.
    [130]Reichstein M, Rey A, Freibauer A, et al. Modeling temporal and large-scale spatial variability of soil respiration from soil water availability, temperature and vegetation productivity indices. Global Biogeochemical Cycles,2003,17:151-1515.
    [131]Reth S, Reichstein M, Falge E. The effect of soil water content, soil temperature, soil pH-value and the root mass on soil CO2 efflux-A modified model. Plant and Soil,2005,268:21-33.
    [132]Rustad L E, Huntington T G, Boone R D. Controls on soil respiration:implications for climate change. Biogeochemistry,2000,48:1-6.
    [133]Sall S, Bertrand I, Chotte J L, et al. Separate effects of the biochemical quality and N content of crop residues on C and N dynamics in soil. Biology and Fertility of Soils,2007,43:797-804.
    [134]Scheel T, Dorfler C, Kalbitz K. Precipitation of dissolved organic matter by aluminum stabilizes carbon in acidic forest soils. Soil Science Society of America Journal,2007,71:64-74.
    [135]Schlesinger W H. On fertilizer-induced soil carbon sequestration in China's croplands. Global Change Biology,2010,16:849-850.
    [136]Schwertmann U, Wagner F, Knicker H. Ferrihydrite-humic associations:magnetic hyperfine interactions. Soil Science Society of America Journal,2005,69:1009-1015.
    [137]Seech A G, Beaucheamp E G. Denitrification in soil aggregates of different sizes. Soil Science Society of America Journal,1988,52:1616-1621.
    [138]Singh K. P, Shekhar C. Seasonal pattern of total soil respiration, its fractionation and soil carbon balance in a wheat-maize rotation cropland at Varanasi. Pedobiologia,1986,29:305-318.
    [139]Singh S, Ghoshal N, Singh K P. Variations in soil microbial biomass and crop roots due to differing resource quality inputs in a tropical dryland agroecosystem. Soil Biology and Biochemistry,2007a,39:76-86.
    [140]Singh S, Ghoshal N, Singh K P. Influence of resource quality of organic inputs on rice-barley dryland agroecosystem:variations in biological productivity, grain yield and efficiency of nitrogen use. Experimental Agriculture,2007b,43:149-161.
    [141]Singh K P, Ghoshal N, Singh S. Soil carbon dioxide flux, carbon sequestration and crop productivity in a tropical dryland agroecosystem:Influence of organic inputs of varying resource quality. Applied Soil Ecology,2009,42:243-253.
    [142]Singh S, Singh J S. Microbial biomass associated with water-stable aggregates in forest, savanna and cropland soils of a seasonally dry tropical region, India. Soil Biology and Biochemistry,1995, 27:1027-1033.
    [143]Sirivedhin T, Gray K A. Factors affecting denitrification rates in experimental wetlands:field and laboratory studies. Ecological Engineering,2006,26:167-181.
    [144]Six J, Elliott E T, Paustian K. Soil macroaggregate turnover and microaggregate formation:a mechanism for C sequestration under no-tillage agriculture. Soil Biology and Biochemistry,2000a, 32:2099-2103.
    [145]Six J, Paustian K, Elliott E T, et al. Soil structure and organic matter I. Distribution of aggregate-size classes and aggregate-associated carbon. Science Society of American Journal, 2000b,64:681-689.
    [146]Six J, Carpentier A, Kessel C, et al. Impact of elevated CO2 on soil organic matter dynamics as related to changes in aggregate turnover and residue quality. Plant and Soil,2001,234:27-36.
    [147]Six J, Conant R T, Paul E A, et al. Stabilization mechanisms of soil organic matter:Implications for C-saturation of soils. Plant and Soil,2002,241:155-176.
    [148]Six J, Bossuyt H, Degryze S, et al. A history of research on the link between (micro)aggregates, soil biota, and soil organic matter dynamics. Soil Tillage Research,2004,79:7-31.
    [149]Six J, Frey S D, Thiet R. K, et al. Bacterial and Fungal Contributions to Carbon Sequestration in Agroecosystems. Soil Science Society of America Journal,2006,70:555-569.
    [150]Skopp J, Jawson M D, Doran J W. Steady-state aerobic microbial activity as a function of soil water content, Soil Science Society of America Journal,1990,54:1619-1625.
    [151]Smith V C, Bradford M A. Litter quality impacts on grassland litter decomposition are differently dependent on soil fauna across time. Applied Soil Ecology,2003,24:197-203.
    [152]Sollins P, Homann P, Caldwell B A. Stabilization and destabilization of soil organic matter: mechanisms and controls. Geoderma,1996,74:65-105.
    [153]Spaccini R, Zena A, Igwe C A, et al. Carbohydrates in water-stable aggregates and particle size fractions of forested and cultivated soils in two contrasting tropical ecosystems. Biogeochemistry, 2001,53:1-22.
    [154]Takai Y. The mechanism of methane fermentation in flooded paddy soil. Soil Science and Plant Nutrition,1970,16:238-244.
    [155]Tate K R, Theng B K G. Organic matter and its interactions with inorganic soil constituents. In: Tate K R, Theng B K G (Eds), Soil with a variable Charge. New Zealand, Society and Soil Science, Lower Hutt,1980, pp 225-249.
    [156]Taylor B R, Parkinson D, Parsons W F J. Nitrogen and lignin content as predictors of litter decay rates:a microcosm test. Ecology,1989,70:97-104.
    [157]Tisdall J M, Oades J M. Organic matter and water-stable aggregates in soils. Journal of Soil Science,1982,33:141-163.
    [158]Thangarajan R, Bolan N S, Tian G L, et al. Role of organic amendment application on greenhouse gas emission from soil. Science of the Total Environment.2013,465:72-96.
    [159]Tournassat C, Greniche J M, Tisserand D. The titration of clay minerals I. Discontinuous back titration technique combined with CEC measurements. Journal of Colloid and Interface Science, 2004,273:224-233.
    [160]Vanlauwe B, Wendt J, Diels J. Combined application of organic matter and fertilizer. In:Tian G, Ishida F, Keatinge J D H (Eds.), Sustaining Soil Fertility in West Africa,58. SSSA, American Society of Agronomy, Madison, WI,2001, pp.247-279.
    [161]Vigil M F, Kissel D E. Equations for estimating the amount of nitrogen mineralized from crop residues. Soil Science Society of America Journal,1991,55:757-761.
    [162]Walkley A., Black L A. An examination of the method for determining soil organic matter, and a proposed modification of the chromic acidtitration method. Soil Science,1934,37:29-38.
    [163]Wander M M, Yang X. Influence of tillage on the dynamics of loose-and occluded particulate and humified organic matter fractions. Soil Biology and Biochemistry,2000,32:1151-1160.
    [164]Wan S Q, Norby R J, Ledford J, et al. Responses of soil respiration to elevated CO2, air warming, and changing soil water availability in a model old-field grassland. Global Change Biology,2007, 13:2411-2424.
    [165]Weier K L, Doran J W, PoWer J F, et al. Denitrification and the dinitrogen/nitrous oxide ratio as affected by soil water, available carbon, and nitrate. Soil Science Society of America Journal,1993, 57:66-72.
    [166]Yakovchenko V P, Sikora L J, Millner P D. Carbon and nitrogen mineralization of added particulate and macroorganic matter. Soil Biology and Biochemistry,1998,30:2139-2146.
    [167]Yang X, Shang Q, Wu P, et al. Methane emissions from double rice agriculture under long-term fertilizing systems in Hunan, China. Agriculture, Ecosystems and Environment,2010, 137:308-316.
    [168]Zanatta J A, Bayer C, Dieckow J, et al. Soil organic carbon accumulation and carbon costs related to tillage, cropping systems and nitrogen fertilization in a subtropical Acrisol. Soil and Tillage Research,2007,94:510-519.
    [169]Zhang A F, Bian R J, Pan G X, et al. Effects of biochar amendment on soil quality, crop yield and greenhouse gas emission in a Chinese rice paddy:A field study of 2 consecutive rice growing cycles. Field Crops Research,2012,127:153-160.
    [170]Zhou P, Song G H, Pan G X, et al. Role of chemical protection by binding to oxyhydrates in SOC sequestration in three typical paddy soils under long-term agro-ecosystem experiments from South China. Geoderma,2009,153:52-60.
    [171]Zhu T B., Zhang J B, Yang W Y, et al. Effects of organic material amendment and water content on NO, N2O, and N2 emissions in a nitrate-rich vegetable soil. Biology and Fertility of Soils,2013, 49:153-163.
    [172]鲍士旦,2000.土壤农化分析,北京:中国农业出版社.
    [173]曹志平,胡诚,叶钟年,等.不同土壤培肥措施对华北高产农田土壤微生物生物量碳的影响[J].生态学报,2006,26(5):1486-1493.
    [174]陈安磊,谢小立,陈惟财,等.长期施肥对红壤稻田耕层土壤碳储量的影响.环境科学,2009,30(5):1267-1272.
    [175]丁维新,蔡祖聪.土壤有机质和外源有机物对甲烷产生的影响.生态学报,2002,22(10):1672-1679.
    [176]杜章留.太行山前平原集约种植区保护性耕作下土壤质量与碳氮固持机制研究.博士论文,2012.
    [177]高旺盛,陈源泉,梁龙.论发展循环农业的基本原理与技术体系.农业现代化研究,2007,28(6):731-734.
    [178]高旺盛.坚持走中国特色的循环农业科技创新之路.农业现代化研究,2010,31(2):129-133.
    [179]郭胜利,吴金水,党廷辉.轮作和施肥对半干旱区作物地上部生物量与土壤有机碳的影响,中国农业科学,2008,41(3):744-751
    [180]古伯贤,赵哲权,王泽文,等.不同有机物养地供肥机制探讨.河北农业科学,1993,(3):15-18.
    [181]黄斌,王敬国,龚元石,等.冬小麦夏玉米农田土壤呼吸与碳平衡的研究,农业环境科学学报,2006,25(1):156-160.
    [182]黄不凡.绿肥、麦秸还田培养地力的研究Ⅰ.对土壤有机质和团聚体性状的影响[J].土壤学报,1984,21(2):113-122.
    [183]黄坚雄,陈源泉,隋鹏,等.农田温室气体净排放研究进展.中国人口资源与环境,2011,8:87-94.
    [184]姜培坤.不同林分下土壤活性有机碳库研究.林业科学,2005,41(1):10-13.
    [185]梁尧,韩晓增,宋春,等.不同有机物料还田对东北黑土活性有机碳的影响.中国农业科学,2011,44(17):3565-3574
    [186]李东坡,武志杰,陈利军,等.长期培肥黑土微生物量碳动态变化及影响因素.应用生态学报,2004,15(8):1334-1338
    [187]李国学,张福锁.固体废物堆肥化与有机复混肥生产.北京:化学工业出版,2000.
    [188]李辉信,袁颖红,黄欠如,等.不同施肥处理对红壤水稻土团聚体有机碳分布的影响.土壤学报,2006,43(3):422-429.
    [189]李江涛,张斌,彭新华.施肥对红壤性水稻土颗粒有机物形成及团聚体稳定性的影响.土壤学报,2004,41(6):912-917.
    [190]李娟,赵秉强,李秀英,等.长期有机无机肥料配施对土壤微生物学特性及土壤肥力的影响.中国农业科学,2008,41(1):144-152.
    [191]李小刚,崔志军,王玲英.施用秸秆对土壤有机碳组成和结构稳定性的影响.土壤学报,2002,39(3):421-428.
    [192]李忠佩,林心雄,车玉萍.中国东部主要农田土壤有机碳库的平衡与趋势分析.土壤学报,2002,39(3):351-360.
    [193]刘满强,胡锋,陈小云.土壤有机碳稳定机制研究进展.生态学报,2007,27(6):2642-2650.
    [194]刘守龙,苏以荣,黄道友,等.微生物商对亚热带地区土地利用及施肥制度的响应.中国农业科学,2006,39(7):1411-1418.
    [195]刘晓雨,李志鹏,潘根兴,等.长期不同施肥下太湖地区稻田净温室效应和温室气体排放强度的变化.农业环境科学学报,2011,30(9):1783-1790.
    [196]刘巽浩,胡跃高,陈阜.粮食—中国农业的永恒难题与主题.农业现代化研究,2010,31(4):385-391.
    [197]刘巽浩,徐文修,李增嘉,等.农田生态系统碳足迹法:误区、改进与应用—兼析中国集约农作碳效率.中国农业资源与区划,2013,34(6):1-11.
    [198]刘巽浩,徐文修,李增嘉,等.农田生态系统碳足迹法:误区、改进与应用—兼析中国集约农作碳效率(续).中国农业资源与区划,2014,35(1):1-7.
    [199]刘贞先,伊晓路,孙立,等.中国生物质废弃物利用现状分析.环境科学与管理,2007,32(2):104-106.
    [200]刘中良,宇万太,周桦,等.不同有机厩肥输入量对土壤团聚体有机碳组分的影响.土壤学报,2011,48(6):1149-1157.
    [201]刘振东,李贵春,杨晓梅,等.我国农业废弃物资源化利用现状与发展趋势分析.安徽农业科学, 2012,40(26):13068-13070,13076.
    [202]马力,杨林章,肖和艾,等.施肥和秸秆还田对红壤水稻土有机碳分布变异及其矿化特性的影响.土壤,2011,43(6):883-890.
    [203]孟磊,丁维新,蔡祖聪,等.长期定量施肥对土壤有机碳储量和土壤呼吸影响.地球科学进展,2005,20(6):687-692.
    [204]孟磊,蔡祖聪,丁维新.长期施肥对华北典型潮土N分配和N2O排放的影响.生态学报,2008,28(12):6197-6203.
    [205]潘根兴,李恋卿,李旭辉,等.中国土壤有机碳库量与农业土壤碳固定动态的若干问题.地球科学进展,2003,18(4):609-618.
    [206]潘根兴,李恋卿,郑聚锋,等.土壤碳循环研究及中国稻田土壤固碳研究的进展与问题.土壤学报,2008,45(5):901-914.
    [207]潘志勇,吴文良,刘光栋,等.不同秸秆还田模式与氮肥施用量对土壤N2O排放的影响.土壤肥料,2004,(5):6-8.
    [208]彭靖.对我国农业废弃物资源化利用的思考.生态环境学报,2009,18(2):794-798.
    [209]秦晓波,李玉娥,刘克樱,等.长期施肥对湖南稻田甲烷排放的影响.中国农业气象,2006,27(1):19-22.
    [210]秦晓波,李玉娥,刘克樱,等.不同施肥处理稻田甲烷和氧化亚氮排放特征.农业工程学报,2006a,22(7):143-148.
    [211]任军,郭金瑞,边秀芝,等.土壤有机碳研究进展.中国土壤与肥料,2009,(6):1-8.
    [212]任天志,Stefano G.持续农业中的土壤生物指标研究.中国农业科学,2000,33(1):68-75
    [213]史磊刚,范士超,孔凡磊,等.华北平原主要作物生产的碳效率研究初报.作物学报,2011,37(8):1485-1490.
    [214]孙瑞莲,朱鲁生,赵秉强,等.长期施肥对土壤微生物的影响及其在养分调控中的作用.应用生态学报,2004,15(10):1907-1910
    [215]孙永明,李国学,张夫道,等.中国农业废弃物资源化现状与发展战略.农业工程学报,2005,21(8):169-173.
    [216]孙振钧,袁振宏,张夫道,等.农业废弃物资源化与农村生物质资源战略研究报告.国家中长期科学和技术发展战略研究,2004.
    [217]孙振钧.中国生物质产业及发展取向.农业工程学报,2004,20(5):1-5.
    [218]孙中林,吴金水,葛体达,等.土壤质地和水分对水稻土有机碳矿化的影响.环境科学,2009,30(1):214-220.
    [219]王峰,王义祥,翁伯琦,等.双胞蘑菇菌渣施用对龙眼园土壤呼吸及可溶性有机碳的影响.福建农业学报,2011,26(2):291-297.
    [220]魏小波,何文清,黎晓峰,等.农田土壤有机碳固定机制及其影响因子研究进展.中国农业气象,2010,31(4):487494.
    [221]卫智涛,周国英,胡清秀.食用菌菌渣利用研究.现状中国食用菌,2010,29(5):3-6,11.
    [222]苑韶峰,杨丽霞.土壤有机碳库及其模型研究进展.土壤通报,2010,41(3):738-743.
    [223]吴庆标,王效科,郭然.土壤有机碳稳定性及其影响因素.土壤通报,2005,36(5):742-747.
    [224]徐建民,赛夫,袁可能.土壤有机矿质复合体研究Ⅸ.钙键复合体和铁铝键复合体中腐殖质的性状特征.土壤学报,1999,36(2):168-178.
    [225]徐明岗,于荣,孙小凤,等.长期施肥对我国典型土壤活性有机质及碳库管理指数的影响.植物营养与肥料学报,2006,12(4):459-465.
    [226]张璐,张文菊,徐明岗,等.长期施肥对中国3种典型农田土壤活性有机碳库变化的影响.中国农业科学,2009,42(5):1646-1655.
    [227]张旭博,徐明岗,张文菊,等.添加有机物料后红壤CO2释放特征与微生物生物量动态.中国农业科学,2011,44(24):5013-5020
    [228]张于光,张小全,肖烨.米亚罗林区土地利用变化对土壤有机碳和微生物量碳的影响.应用生态学报,2006,17(11):2029-2033
    [229]赵红,吕贻忠,杨希,等.不同配肥方案对黑土有机碳含量及碳库管理指数的影响.中国农业科学,2009,42(9):3164-3169.
    [230]周萍,潘根兴,李恋卿,等.南方典型水稻土长期试验下有机碳积累机制V碳输入与土壤碳固定.中国农业科学,2009,42(12):4260-4268.
    [231]周卫军,王凯荣,郝金菊,等.红壤稻田生态系统有机物料循环对土壤有机碳转化的影响.生态学杂志,2006,25(2):140-144.
    [232]邹建文,黄耀,宗良纲,等.稻田不同种类有机肥施用对后季麦田N20排放的影响.环境科学,2006,27(7):1264-1268.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700