免耕和稻草覆盖对红壤旱地土壤物理性质及玉米产量的影响
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  • 英文篇名:Effects of No-tillage and Rice Straw Mulching on Soil Physical Properties and Maize Yield in Red Soil Dryland
  • 作者:杨贺菲 ; 赵静 ; 张旭
  • 英文作者:YANG He-fei;ZHAO Jing;ZHANG Xu;Changjiang River Scientific Research Institute;Hubei Academy of Environmental Sciences;
  • 关键词:红壤旱地 ; 免耕 ; 稻草覆盖 ; 土壤物理性质 ; 玉米产量
  • 英文关键词:Red soil dryland;;No-tillage;;Rice straw mulching;;Soil physical property;;Maize yield
  • 中文刊名:JXNY
  • 英文刊名:Acta Agriculturae Jiangxi
  • 机构:长江科学院;湖北省环境科学研究院;
  • 出版日期:2018-10-15
  • 出版单位:江西农业学报
  • 年:2018
  • 期:v.30
  • 基金:国家科技支撑计划项目(2012BAH33B00)
  • 语种:中文;
  • 页:JXNY201810010
  • 页数:5
  • CN:10
  • ISSN:36-1124/S
  • 分类号:49-53
摘要
通过设置常规耕作(CT)、常规耕作+稻草覆盖、免耕、免耕+稻草覆盖4个处理,研究了免耕和稻草覆盖对红壤旱地土壤物理性及玉米产量的影响,并分析了玉米产量与土壤物理性质间的相关性。结果表明:与常规耕作相比,免耕增加了0~20 cm土层土壤容重和0~30 cm土层土壤紧实度,并降低了0~20 cm土层土壤饱和持水量和非毛管孔隙度;稻草覆盖对土壤容重、水分常数及孔隙状况有一定的改善作用,但影响较小;相比于常规耕作,免耕造成了玉米产量的下降,而稻草覆盖则提高了玉米产量;玉米产量与表层土壤物理性质的相关性较好,其受土壤容重、饱和持水量、非毛管孔隙度、总孔隙度的影响较大。
        The effects of no-tillage and rice straw mulching on the soil physical properties and maize yield in red soil dryland were investigated by setting four treatments,including conventional tillage( CT),conventional tillage + rice straw mulching( CT+M),no-tillage( NT),and no-tillage + rice straw mulching( NT+M),and the correlations between the soil physical properties and maize yield were also analyzed. The results showed that: as compared with the conventional tillage,the soil bulk density in 0~ 20 cm soil layer and the soil compactness in 0 ~ 30 cm soil layer were increased by the no-tillage treatment,while the soil saturated water-holding capacity and non-capillary porosity in 0 ~ 20 cm soil layer were decreased; rice straw mulching could slightly improve soil bulk density,soil moisture parameters and soil porosity,but its influences were less. In comparison with the conventional tillage,the no-tillage treatment reduced maize yield,while rice straw mulching increased maize yield. Maize yield was closely correlated with the physical properties of surface soil,and it was greatly influenced by the soil bulk density,saturated water-holding capacity,non-capillary porosity and total porosity.
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