吉林西部不同种植年限水稻土酸缓冲性能研究
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摘要
种植水稻是盐碱地区改良土壤的一种有效方式,而选取p H值较低的水稻苗床土已经成为盐碱地区亟待解决的一个主要问题。本文主要针对吉林省西部盐碱地区不同种植年限的水稻土进行理化性质、水溶性盐基离子和酸缓冲性能的测定,确定影响盐渍水稻土酸缓冲性的主要因素,寻找水稻育苗土可利用资源。结果表明:西部不同种植年限盐渍水稻土的酸缓冲容量表现为:种植60年(壤质黏土)<50年(壤质黏土)<35年(壤质黏土)<45年(壤质黏土)<20年(壤质黏土)<45年(黏土)<25年(黏土),酸缓冲性主要受土壤碳酸盐、土壤黏粒及土壤碱化度的影响,种植50年和60年水稻的壤质粘土酸缓冲性较弱,易于调酸,可以考虑作为苗床土的供选资源。
Rice cultivation was an effective way to improve the soil in saline areas. However, how to select the riceseedbed soil has become a major problem in saline areas. Focused on the different cultivation years of paddy soils,the acid buffering properties, water soluble inorganic salt ions and physical and chemical properties were analyzedto find the key factors for acid buffering properties. The results showed that the acid buffering capacities of salinepaddy soil was 60 years of loamy clay < 50 years of loamy clay < 35 years of loamy clay < 45 years of loamy clay <20 years of loamy clay < 45 years of clay < 25 years of clay. The content of CO32-, clay particles and ESP played theimportant roles in the soil acid buffering ability, and the acid buffering capacity of planting 50 years and 60 years ofloamy clay were weaker than others, and their acidity were easy to regulate and control, which could be developed asseedbed soil.
Rice cultivation was an effective way to improve the soil in saline areas. However, how to select the riceseedbed soil has become a major problem in saline areas. Focused on the different cultivation years of paddy soils,the acid buffering properties, water soluble inorganic salt ions and physical and chemical properties were analyzedto find the key factors for acid buffering properties. The results showed that the acid buffering capacities of salinepaddy soil was 60 years of loamy clay < 50 years of loamy clay < 35 years of loamy clay < 45 years of loamy clay <20 years of loamy clay < 45 years of clay < 25 years of clay. The content of CO32-, clay particles and ESP played theimportant roles in the soil acid buffering ability, and the acid buffering capacity of planting 50 years and 60 years ofloamy clay were weaker than others, and their acidity were easy to regulate and control, which could be developed asseedbed soil.
引文
[1]程式华,胡培松.中国水稻科技发展战略[J].中国水稻科学,2008,22(3):223-226.
[2]Zhang X,Wang D,Fang F,et al.Food safety and rice production in China[J].Resource Agricultural Modernization,2005,26(1):85-88.
[3]Wen-Yi Dong,Xin-Yu Zhang,Xiao-Qin Dai.Changes in soil microbial community composition in response to fertilization of paddy soils in subtropical China[J].Applied Soil Ecology,2014(84):140-147.
[4]李凯,王勇,窦森.吉林省西部土地开发整理重大工程与苏打盐碱地工程改良[J].吉林农业科学,2009,34(1):20-24.
[5]王春裕,王汝镛,李建东.中国东北地区盐渍土的生态分布[J].土壤通报,1999,30(5):193-196.
[6]王春裕,武志杰,石元亮,等.中国东北地区的盐渍土资源[J].土壤通报,2004,35(5):643-647.
[7]赵兰坡,冯君,王宇,等.松嫩平原盐碱地种稻开发的理论与技术问题[J].吉林农业大学学报,2012,34(3):237-241.
[8]张永春,汪吉东,沈明星,等.长期不同施肥对太湖地区典型土壤酸化的影响[J].土壤学报,2010,47(3):465-472.
[9]徐仁扣,Coventry D R.某些农业措施对土壤酸化的影响[J].农业环境保护,2002,21(5):385-388.
[10]王兴样,李清曼,曹慧,等.关于植物对红壤的酸化作用及其致酸机理[J].土壤通报,2004,35(1):73-77.
[11]刘付程,史学正,于东升.近20年来太湖流域典型地区土壤酸度的时空变异特征[J].长江流域资源与环境,2004,15(6):740-744.
[12]李彬,王志春,马红媛,等.吉林省盐碱地资源与可持续利用对策[J].吉林农业科学,2005,30(5):46-50.
[13]Xu R K,Coventry D R,Farhoodi A,et al.Soil acidification as influenced by crop rotations,stubble management,and application of nitrogenous fertilizer,Tarlee,South Australia[J].Australian Journal of Soil Research,2003,40(3):483-496.
[14]Xu R,Zhao A,Li Q,et al.Acidity regime of the red soils in a subtropical region of southern China under field conditions[J].Geoderma,2003(115):75-84.
[15]李建国,章明奎,周翠.浙江省农业土壤酸缓冲性能的研究[J].浙江农业学报,2005,17(4):207-211.
[16]陈翠玲,蒋爱凤,任秀娟.潮土地区不同质地类型土壤对酸缓冲性能的研究[J].河南农业科学,2005(10):64-65.
[17]汪吉东,戚冰洁,张永春,等.长期施肥对砂壤质石灰性潮土土壤酸碱缓冲体系的影响[J].应用生态学报,2012,23(4):1031-1036.
[18]鲍士旦.土壤农化分析[M].北京:中国农业出版社,178-200.
[19]刘伟,尚庆昌.长春地区不同类型土壤的缓冲性及其影响因素[J].吉林农业大学学报,2001,23(3):78-82.
[20]尚庆昌,徐丽.水稻苗床土酸度调节的研究[J].吉林农业大学学报,1983(1):73-85.
[21]宫绍斌,郑长艳.水稻旱育苗中立枯病的综合防治[J].农业与技术,2001,2(1):45-47.
[22]杨宁,姜亦梅,赵兰坡.吉林省西部不同利用方式苏打盐碱土的缓冲性能研究[J].中国农学通报,2010,26(18):196-200.
[23]王文婧,戴万宏.安徽主要土壤酸碱性及其酸缓冲性能研究[J].中国农学通报,2012,28(15):67-72.
[24]赵国臣,齐春艳,侯立刚,等.吉林省苏打盐碱地水稻生产历史进程与展望[J].沈阳农业大学学报,2012,43(6):673-680.
[25]Weaver A R,Kissel D E,Chen F,et al.Mapping soil p H buffering capacity of selected fields in the coastal plain[J].Soil Science Society of America Journal,2004(68):662-668.
[26]Aitken R L,Moody P W.The effect of valence and ionic strength on the measurement of p H buffer capacity[J].Australian Journal of Soil Research,1994(32):975-984.
[27]黄平,张佳宝,朱安宁,等.黄淮海平原典型潮土的酸碱缓冲性能[J].中国农业科学,2009,42(7):2392-2396.
[28]廖柏寒,戴昭华.土壤对酸沉降的缓冲能力与土壤矿物的风化特征[J].环境科学学报,1991,4(11):423-430.
[29]王楠,赵兰坡,周彦明,等.玉米(超)高产与普通生产田土壤酸碱缓冲作用的研究[J].吉林农业科学,2009,34(2):24-27.
[2]Zhang X,Wang D,Fang F,et al.Food safety and rice production in China[J].Resource Agricultural Modernization,2005,26(1):85-88.
[3]Wen-Yi Dong,Xin-Yu Zhang,Xiao-Qin Dai.Changes in soil microbial community composition in response to fertilization of paddy soils in subtropical China[J].Applied Soil Ecology,2014(84):140-147.
[4]李凯,王勇,窦森.吉林省西部土地开发整理重大工程与苏打盐碱地工程改良[J].吉林农业科学,2009,34(1):20-24.
[5]王春裕,王汝镛,李建东.中国东北地区盐渍土的生态分布[J].土壤通报,1999,30(5):193-196.
[6]王春裕,武志杰,石元亮,等.中国东北地区的盐渍土资源[J].土壤通报,2004,35(5):643-647.
[7]赵兰坡,冯君,王宇,等.松嫩平原盐碱地种稻开发的理论与技术问题[J].吉林农业大学学报,2012,34(3):237-241.
[8]张永春,汪吉东,沈明星,等.长期不同施肥对太湖地区典型土壤酸化的影响[J].土壤学报,2010,47(3):465-472.
[9]徐仁扣,Coventry D R.某些农业措施对土壤酸化的影响[J].农业环境保护,2002,21(5):385-388.
[10]王兴样,李清曼,曹慧,等.关于植物对红壤的酸化作用及其致酸机理[J].土壤通报,2004,35(1):73-77.
[11]刘付程,史学正,于东升.近20年来太湖流域典型地区土壤酸度的时空变异特征[J].长江流域资源与环境,2004,15(6):740-744.
[12]李彬,王志春,马红媛,等.吉林省盐碱地资源与可持续利用对策[J].吉林农业科学,2005,30(5):46-50.
[13]Xu R K,Coventry D R,Farhoodi A,et al.Soil acidification as influenced by crop rotations,stubble management,and application of nitrogenous fertilizer,Tarlee,South Australia[J].Australian Journal of Soil Research,2003,40(3):483-496.
[14]Xu R,Zhao A,Li Q,et al.Acidity regime of the red soils in a subtropical region of southern China under field conditions[J].Geoderma,2003(115):75-84.
[15]李建国,章明奎,周翠.浙江省农业土壤酸缓冲性能的研究[J].浙江农业学报,2005,17(4):207-211.
[16]陈翠玲,蒋爱凤,任秀娟.潮土地区不同质地类型土壤对酸缓冲性能的研究[J].河南农业科学,2005(10):64-65.
[17]汪吉东,戚冰洁,张永春,等.长期施肥对砂壤质石灰性潮土土壤酸碱缓冲体系的影响[J].应用生态学报,2012,23(4):1031-1036.
[18]鲍士旦.土壤农化分析[M].北京:中国农业出版社,178-200.
[19]刘伟,尚庆昌.长春地区不同类型土壤的缓冲性及其影响因素[J].吉林农业大学学报,2001,23(3):78-82.
[20]尚庆昌,徐丽.水稻苗床土酸度调节的研究[J].吉林农业大学学报,1983(1):73-85.
[21]宫绍斌,郑长艳.水稻旱育苗中立枯病的综合防治[J].农业与技术,2001,2(1):45-47.
[22]杨宁,姜亦梅,赵兰坡.吉林省西部不同利用方式苏打盐碱土的缓冲性能研究[J].中国农学通报,2010,26(18):196-200.
[23]王文婧,戴万宏.安徽主要土壤酸碱性及其酸缓冲性能研究[J].中国农学通报,2012,28(15):67-72.
[24]赵国臣,齐春艳,侯立刚,等.吉林省苏打盐碱地水稻生产历史进程与展望[J].沈阳农业大学学报,2012,43(6):673-680.
[25]Weaver A R,Kissel D E,Chen F,et al.Mapping soil p H buffering capacity of selected fields in the coastal plain[J].Soil Science Society of America Journal,2004(68):662-668.
[26]Aitken R L,Moody P W.The effect of valence and ionic strength on the measurement of p H buffer capacity[J].Australian Journal of Soil Research,1994(32):975-984.
[27]黄平,张佳宝,朱安宁,等.黄淮海平原典型潮土的酸碱缓冲性能[J].中国农业科学,2009,42(7):2392-2396.
[28]廖柏寒,戴昭华.土壤对酸沉降的缓冲能力与土壤矿物的风化特征[J].环境科学学报,1991,4(11):423-430.
[29]王楠,赵兰坡,周彦明,等.玉米(超)高产与普通生产田土壤酸碱缓冲作用的研究[J].吉林农业科学,2009,34(2):24-27.