邵建荣,张凤华,董 艳,李乐佳,赵 宇,张敬远,胡治强,徐 秀.干旱区微咸水滴灌条件下典型土壤盐碱化影响因素研究[J].干旱地区农业研究,2015,33(6):216~221
干旱区微咸水滴灌条件下典型土壤盐碱化影响因素研究
Influence factors research of typical soil salinization and alkalization under brackish water drip irrigation in arid areas
  
DOI:10.7606/j.issn.1000-7601.2015.06.36
中文关键词:  微咸水  滴灌  土壤盐碱化  土壤离子  干旱区
英文关键词:brackish water  drip irrigation  soil salinization and alkalization  soil ion  arid area
基金项目:教育部科学技术研究项目(213039A);国家自然科学基金项目(31360320);国家科技支撑项目(2014BAC14B03)
作者单位
邵建荣 石河子大学农学院 新疆 石河子 832003新疆兵团绿洲生态农业重点实验室 新疆 石河子 832003 
张凤华 石河子大学农学院 新疆 石河子 832003新疆兵团绿洲生态农业重点实验室 新疆 石河子 832003 
董 艳 石河子大学农学院 新疆 石河子 832003 
李乐佳 石河子大学农学院 新疆 石河子 832003 
赵 宇 石河子大学农学院 新疆 石河子 832003 
张敬远 石河子大学农学院 新疆 石河子 832003 
胡治强 石河子大学农学院 新疆 石河子 832003 
徐 秀 石河子大学农学院 新疆 石河子 832003 
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中文摘要:
      以代表性的沙壤和黏壤棉田土壤为研究对象,分别利用高、低矿化度水进行5年灌溉,即黏壤-低矿化度,黏壤-高矿化度,沙壤-低矿化度,沙壤-高矿化度共四个处理,测定0~100 cm分层土样总盐、pH、Na+、K+、Ca2+、Mg2+、SAR、ESP等指标,以研究玛纳斯河流域冲积扇扇缘和干三角洲区不同浓度微咸水长期滴灌条件下土壤盐分、土壤碱度、主要阳离子的变化,探讨对土壤盐化和碱化产生主要影响的离子,为干旱区微咸水灌溉生态安全管理提供理论参考。结果表明:冲积扇扇缘带黏壤土和干三角洲沙壤土盐化和碱化相伴发生,且主要受灌溉水矿化度影响;对土壤盐化和碱化均产生主要影响的离子为Na+,对土壤盐分产生主要影响的离子为Na+与Ca2+。这表明玛纳斯河流域土壤盐碱化的治理应从降低灌溉水Na+入手,将控制灌溉水总盐分和降低Na+占比结合起来,达到既降盐又防治土壤持续碱化的目的。
英文摘要:
      In order to study the change of soil salinity, soil alkalinity and main cations under long time drip irrigation with different concentration of brackish water in alluvial fan of the edge and the dry delta area in Manas River Basin, taking the representative sandy loam and clay loam soil in cotton field as the research object, using the high and low saline water for 5 years irrigation, has set up four treatments as clay loam-low salinity, clay loam-high salinity, sandy loam-low salinity and sandy loam-high salinity, measured the soil total salt, pH, Na+, K+, Ca2+, Mg2+, SAR, ESP, etc. in 0~100 cm soil layers, discussed the ions that have produced the main impact to soil salinization and alkalization, to provide the theoretical reference of ecological security for brackish water irrigation in arid area. The results indicated that: The soil salinization and alkalization in clay loam of alluvial fan of the edge and sandy loam of the dry delta area was together occurred, also was mainly affected by irrigation water salinity. The ion of main influence for soil salinization and soil alkalization was Na+ and for soil salinization was Na+ and Ca2+. It indicated that amelioration of the soil salinization in Manas River Basin should be started with reducing irrigation water Na+, and combined control of total salt content in irrigation water with reducng the proportion of Na+ to achieve the purpose of reducing salt and preventing and controlling soil alkalization.
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