Advance in Studies on Effect of Mulched Drip Irrigation on Production and Emission of Greenhouse Gas

doi:10.11924/j.issn.1000-6850.2012-0296

Abstract

Abstract: CO₂, CH₄ and N₂O have attracted increasing attention as great contributors to global warming. Mulched drip irrigation is also receiving wide interests as a water-saving agricultural technology. Research on the influence of soil temperature and moisture on production and emission of greenhouse gases (GHG), changes of soil temperature and moisture caused by mulched drip irrigation and their effects on emission of GHG were summarized in this paper. Research results demonstrated that: (1) soil temperature and moisture had an influence on production and emission of GHG by affecting soil microbial activity, soil aeration and gas transmission rate; (2) Emission rate of soil CO₂ was positively related to topsoil temperature of superficial layer, the production of both CH₄ and N₂O had a certain optimum temperature, and the relation between the oxidation of CH₄ and temperature was various; (3) Soil moisture’s effect on production and oxidation of CH₄ and the production of N₂O was greater than soil temperature, rate of methane oxidation was negatively related to soil moisture, while the emission of CO₂ and N₂O had an optimum moisture range; (4) The temperature-increasing and humidity-preserving effect, the barrier effect of gaseous transmission caused by mulch and the partially soil wetting pattern under drip irrigation would have an influence on the production and emission of GHG. In the end, several relevant research aspects left to be developed and perfected were summarized and presented: how to reduce GHG emission by confirming and controlling the wetting percentage of soil; how to quantify the combined effect of mulch and drip irrigation; how to regulate and control crops’process of growth through regulating soil CO₂ emission.

References

[1] IPCC. Changes in Atmospheric Constituents and in Radiative Forcing[R].2007.
[2] IPCC. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change[R]. Cambridge: Cambridge University Press,2007.
[3] IPCC. Greenhouse Gas Mitigation in Agriculture[R].2006.
[4] 宋秋华,李凤民,王俊,等.覆膜对春小麦农田微生物数量和土壤养分的影响[J].生态学报,2002,22(12):2125-2132.
[5] 丁维新,蔡祖聪.温度对土壤氧化大气CH4的影响[J].生态学杂志, 2003,22(3):54-58.
[6] Dobbie K E, Smith K A. The effects of temperature, water-filled pore space and land use on N2O emissions from an imperfectly drained gleysol[J].European Journal of Soil Science,2001,52(4): 667-673.
[7] 罗辑,杨忠,杨清伟.贡嘎山东坡峨眉冷杉林区土壤CO2排放[J].土壤学报,2000,37(3):402-409.
[8] 李虎,邱建军,王立刚.农田土壤呼吸特征及根呼吸贡献的模拟分析[J].农业工程学报,2008,24(4):14-20.
[9] 张东秋,石培礼,何永涛,等.西藏高原草原化小嵩草草甸生长季土壤微生物呼吸测定[J].自然资源学报,2006,21(3):458-464.
[10] 周志田,成升魁,刘允芬,等.中国亚热带红壤丘陵区不同土地利用方式下土壤 CO2排放规律初探[J].资源科学,2002,24(2):83-87.
[11] Jabro J D, Sainju U, Stevens W B, et al. Carbon dioxide fl ux as affected by tillage and irrigation in soil converted from perennial forages to annual crops[J].Journal of Environmental Management, 2008,88(4):1478-1484.
[12] S?nger A, Geisseler D, Ludwig B. Effects of moisture and temperature on greenhouse gas emissions and C and N leaching losses in soil treated with biogas slurry[J].Biol Fert Soils,2011,47: 249-259.
[13] 胡启武,吴琴,李东,等.不同土壤水分含量下高寒草地 CH4释放的比较研究[J].生态学杂志,2005,24(2).
[14] 孙向阳.北京低山区森林土壤中 CH4排放通量的研究[J].土壤与环境,2000,9(3):173-176.
[15] Priemer A, Christensen S. Seasonal and spatial variation of methane oxidation in a Danish spruce forest[J].Soil Biology & Biochemistry, 1997(29):1165-1172.
[16] Flessa H, Dorsch P. Seasonal variation of N2O and CH4 fluxes in differently managed arable soils in southern Germany[J]. Geophysical Research Letters,1995,97(D11):23115-23124.
[17] 董云社,章申,齐玉春,等.内蒙古典型草地 CO2, N2O, CH4通量的同时观测及其日变化[J].科学通报,2000(3):318-322.
[18] Del Grosso S J, Parton W J, Mosier A R, et al. General CH4 oxidation model and comparisons of CH4 oxidation in natural and managed systems[J].Global Biogeochemical Cycles,2000,14(4): 999-1019.
[19] Dunfield P, Knowles R, Dumont R, et al. Methane production and consumption in temperate and subarctic peat soils: response to temperature and pH[J].Soil Biology and Biochemistry,1993,25(3): 321-326.
[20] Conrad R. Soil microorganisms as controllers of atmospheric trace gases (H2, CO, CH4, OCS, N2O, and NO) [J].Microbiological Reviews,1996,60(4):609-640.
[21] Butterbach-Bahl K, Papen H. Four years continuous record of CH4-exchange between the atmosphere and untreated and limed soil of a N-saturated spruce and beech forest ecosystem in Germany[J]. Plant and Soil,2002,240(1):77-90.
[22] 谢军飞,李玉娥.农田土壤温室气体排放机理与影响因素研究进展[J].中国农业气象,2002,23(4):48-53.
[23] 郑循华,王明星,王跃思,等.温度对农田 N2O产生与排放的影响[J].环境科学,1997,18(5):1-6.
[24] Liu C, Zheng X, Zhou Z, et al. Nitrous oxide and nitric oxide emissions from an irrigated cotton field in Northern China[J].Plant Soil,2010,332(1/2):123-134.
[25] Borken W, Davidson E A, Savage K, et al. Effect of summer through fall exclusion, summer drought, and winter snow cover on methane fluxes in a temperate forest soil[J].Soil Biology & Biochemistry,2006,38(6):1388-1395.
[26] 陈全胜,李凌浩,韩兴国,等.水分对土壤呼吸的影响及机理[J].生态学报,2003,23(5):972-978.
[27] 毕建杰,王琦,张衍华,等.施肥对不同品种麦田 CO2通量的影响[J].中国农学通报,2006,22(6):459-463.
[28] Kucera C L, Kirkham D R. Soil respiration studies in tall grass prairie in Missouri[J].Ecology,1971,52(5):912-915.
[29] Borken W, Matzner E. Reappraisal of drying and wetting effects on C and N mineralization and fluxes in soils[J].Global Change Biology,2009,15(4):808-824.
[30] 郝庆菊,王跃思,江长胜,等.湿地甲烷排放研究若干问题的探讨[J].生态学杂志,2005,24(2):170-175.
[31] 何婷婷,华珞,张振贤,等.影响农田土壤有机碳释放的因子及固碳措施[J].首都师范大学学报:自然科学版,2007(01):66-72.
[32] 丁维新,蔡祖聪.土壤甲烷氧化菌及水分状况对其活性的影响[J].中国生态农业学报,2003,11(1):94-97.
[33] Striegl R G. Diffusional limits to the consumption of atmospheric methane by soils[J].Chemosphere,1993,26(1/4):715-720.
[34] Khalil M I, Baggs E M. CH4 oxidation and N2O emissions at varied soil water-filled pore spaces and headspace CH4 concentrations[J]. Soil Biology & Biochemistry,2005,37(10):1785-1794.
[35] Davidson E A. Fluxes of nitrous oxide and nitric oxide from terrestrial ecosystems. In: Rogers, J.E., Whitman, W.B. (Eds.), Microbial Production and Consumption of Greenhouse Gases: Methane, Nitrogen Oxides and Halomethanes[J].American Society of Microbiology,1991:219-235.
[36] Ruser R, Flessa H, Russow R, et al. Emission of N2O, N2 and CO2 from soil fertilized with nitrate: effect of compaction, soil moisture and rewetting[J].Soil Biology & Biochemistry,2006,38(2):263-274.
[37] 郑循华,王明星,王跃思,等.稻麦轮作生态系统中土壤湿度对 N2O产生与排放的影响[J].应用生态学报,1996,7(3):273-279.
[38] 蔡祖聪,Mosier Arivnr.土壤水分状况对 CH4氧化,N2O 和 CO2排放的影响[J].土壤,1999(6):289-294.
[39] 徐文彬,刘广深,刘维屏.降雨和土壤湿度对贵州旱田土壤 N2O释放的影响[J].应用生态学报,2002,13(1):67-70.
[40] 梁东丽,同延安,Emteryd Ove,等.干湿交替对旱地土壤 N2O气态损失的影响[J].干旱地区农业研究,2002,20(2):28-31.
[41] 王凤新,康跃虎,刘士平.滴灌条件下马铃薯耗水规律及需水量的研究[J].干旱地区农业研究,2005,23(1):9-15.
[42] Hou X Y, Wang F X, Han J J, et al. Duration of plastic mulch for potato growth under drip irrigation in an arid region of Northwest China[J].Agricultural And Forest Meteorology,2010,150(1): 115-121.
[43] 龙攀,黄璜.作物覆膜温室效应研究进展[J].作物研究,2010,24(1): 52-55.
[44] 王俊,李凤民,宋秋华,等.地膜覆盖对土壤水温和春小麦产量形成的影响[J].应用生态学报,2003,14(2):205-210.
[45] 张治,田富强,钟瑞森,等.新疆膜下滴灌棉田生育期地温变化规律[J].农业工程学报,2011,27(1):44-51.
[46] 侯晓燕,王凤新,康绍忠,等.西北旱区民勤绿洲滴灌马铃薯揭膜效应研究[J].干旱地区农业研究,2008,26(4):88-93.
[47] 张鑫,蔡焕杰,邵光成,等.膜下滴灌的生态环境效应研究[J].灌溉排水,2002,21(2):1-4.
[48] 杨俊峰,龚月桦,李生秀.旱地小麦覆膜的生理生态效应研究进展[J].陕西农业科学,2009(05):79-82.
[49] Wang D, Shannon M C, Grieve C M, et al. Soil water and temperature regimes in drip and sprinkler irrigation, and implications to soybean emergence[J].Agricultural Water Management,2000,43:15-28.
[50] 姬景红,张玉龙,张玉玲,等.灌溉方法对保护地土壤有机氮矿化特性的影响[J].土壤学报,2009,46(5):869-877.
[51] Li Z, Zhang R, Wang X, et al. Carbon Dioxide Fluxes and Concentrations in a Cotton Field in Northwestern China: Effects of Plastic Mulching and Drip Irrigation[J].Pedosphere,2011,21(2): 178-185.
[52] Jiang P, Wang H, Wu J, et al. Winter mulch increases soil CO2 efflux under Phyllostachys praecox stands[J].Journal of Soil and Sediments,2009,9(6):511-514.
[53] 李世清,李东方,李凤民,等.半干旱农田生态系统地膜覆盖的土壤生态效应[J].西北农林科技大学学报:自然科学版,2003,31(5): 21-29.
[54] 魏虹.地膜覆盖对半干旱区春小麦光合作用及产量的影响[J].西南师范大学学报:自然科学版,2000,25(5):621-625.
[55] 韩建刚,白红英,曲东.地膜覆盖对土壤中N2O排放通量的影响[J].中国环境科学,2002,22(3):95-97.
[56] 朱咏莉,吴金水,韩建刚.地膜覆盖对土壤中N2O释放的影响[J].农业工程学报,2004,20(3):222-225.
[57] 刘岳燕.水分条件与水稻土壤微生物生物量、活性及多样性的关系研究[D].杭州:浙江大学,2009:71-79.
[58] Kallenbach C M, Rolston D E, Horwath W R. Cover cropping affects soil N2O and CO2 emissions differently depending on type of irrigation[J].Agriculture Ecosystems & Environment,2010,137(3/4): 251-260.
[59] Sanchez-Martin L, Arce A, Benito A, et al. Influence of drip and furrow irrigation systems on nitrogen oxide emissions from a horticultural crop[J].Soil Biology & Biochemistry,2008,40(7): 1698-1706.
[60] Scheer C, Qassmann R, Kienzler K, et al. Nitrous oxide emissions from fertilized, irrigated cotton (Gossypium hirsutum L.) in the Aral Sea Basin, Uzbekistan: In fl uence of nitrogen applications and irrigation practices[J].Soil Biology & Biochemistry,2008,2(40): 290-301.
[61] Chapuis-Lardy L, Wrage N, Metay A, et al. Soils, a sink for N2O? A review[J].Global Change Biology,2007,13(1):1-17.