首页 | 本学科首页   官方微博 | 高级检索  
     

耕作与秸秆还田深度变化对不同土层团聚体稳定性的影响
引用本文:于洪久,王根林,段衍,刘峥宇,时妍,刘沣漫,王伟,邱广伟,孙磊,李玉梅. 耕作与秸秆还田深度变化对不同土层团聚体稳定性的影响[J]. 中国土壤与肥料, 2024, 0(1): 1-7
作者姓名:于洪久  王根林  段衍  刘峥宇  时妍  刘沣漫  王伟  邱广伟  孙磊  李玉梅
作者单位:黑龙江省黑土保护利用研究院,农业农村部黑土地保护与利用重点实验室,黑龙江 哈尔滨 150086;中国科学院合肥物质科学研究院,安徽 合肥 230031;黑龙江省绥滨农场,黑龙江 绥滨 156299;黑龙江北大荒现代农业服务集团有限公司宝泉岭分公司,黑龙江 佳木斯 154211;黑龙江省农业科学院克山分院,黑龙江 齐齐哈尔 161601
基金项目:基金项目:国家重点研发计划项目(2022YFD1500305、2022YFD1500704、2016YFD0300806);国家大豆产业技术体系(CARS-04-01A)。
摘    要:耕作和秸秆还田可以改变土壤理化性状,影响土壤团聚体的稳定性。采用田间定位试验,研究耕作与秸秆还田深度变化对旱地草甸土不同深度土层水稳性团聚体稳定性的影响,为科学开展秸秆还田培肥土壤提供依据。结果表明:土壤团聚体稳定性受>2000μm粒径大团聚体影响较大,连续5年翻耕显著降低了表层(0~20 cm)土壤>2000μm粒径水稳性大团聚体的占比,增加了53~250μm微团聚体和<53μm黏粉粒的比例。浅翻(ST)和秸秆浅翻还田(STS)与深翻(DT)和秸秆深翻还田(DTS)分别对10~20和20~30 cm土层黏粉粒的增加影响较大,其中,10~20 cm土层ST较免耕(NT)和DT处理分别增加86.21%和14.65%,20~30 cm土层DT较NT和ST处理分别增加113.82%和59.68%,差异显著(P<0.05);连续翻耕由于对亚耕层(20~40 cm)的频繁扰动,导致250~2000μm粒径团聚体的稳定性降低,DT较NT和ST与DTS处理较覆盖免耕(NTS)和STS处理分别平均降低19.43%与20.57%,且差异显著(P<0.05)。研究结果表明,连...

关 键 词:秸秆还田  耕作  水稳性团聚体  稳定性  土壤深度
收稿时间:2023-01-05

Effects of different tillage and straw returning depths on soil aggregate stability of different soil layers
YU Hong-jiu,WANG Gen -lin,DUAN Yan,LIU Zheng -yu,SHI Yan,LIU Feng -man,WANG Wei,QIU Guang -wei,SUN Lei,LI Yu -mei. Effects of different tillage and straw returning depths on soil aggregate stability of different soil layers[J]. Soil and Fertilizer Sciences, 2024, 0(1): 1-7
Authors:YU Hong-jiu  WANG Gen -lin  DUAN Yan  LIU Zheng -yu  SHI Yan  LIU Feng -man  WANG Wei  QIU Guang -wei  SUN Lei  LI Yu -mei
Affiliation:Heilongjiang Black Soil Conservation and Utilization ResearchInstitute,Key Laboratoryof Black Land Protection and Utilization of Ministry of Agriculture and RuralAreas,Harbin Heilongjiang150086;Hefei Institute of Material Science of ChineseAcademy ofSciences,Hefei Anhui230031;Heilongjiang SuibinFarm,SuibinHeilongjiang156299;Bao Quanling Branch of Heilongjiang Beidahuang Modern Agricultural ServiceCo.,Ltd,JiamusiHeilongjiang154211;Keshan Branch of Heilongjiang Academy of AgriculturalSciences,Qiqihar Heilongjiang161601
Abstract:Tillage and straw returning could change the stability of soil aggregates and physicalcharacteristics. The field positioning experiment was conducted to study the influence of tillage and straw returning depth on the stability of soil water-stable aggregates so as to provide a scientific basis for straw returning depth on dry meadowsoil. The results showed that stability of aggregates was affected by the proportion of macro-aggregates with grain size >2000 μm. The water-stable macro-aggregates with grain size >2000 μm in 0-20 cm soil layer was significantly decreased but contents of 53-250 μm micro-aggregates and clay silt particles <53 μm were increased with constantly tillage in fiveyears.Amongthem,clay silt particles <53μm with shallow tillage in 10-20 cm soil layer increased by 86.21% and14.65%,respectively,compared with no tillage and deeptillage, and deep tillage in 20-30 cmsoil layer increased by 113.82% and59.68%,respectively,compared with no tillage and shallow tillage(P<0.05).Deep tillage had a great impact on the reduction of 250-2000 μm particle size aggregates in 20-40 cm soillayer,which was19.43% and 20.57% onaverage,respectively,lower than no tillage and shallowtillage,straw mulching and straw shallow returning withsignificantdifferences( P<0.05).The stability of aggregates was reduced due to the disturbance of continuous deep tillage to thesubsoil,all of these can provide a scientific basis to improve the soil structural properties and the stability of aggregates and fertilize thesoil,and the depth of tillage and straw returning should be adjusted by means of rotation in future production.
Keywords:strawreturning;tillage;water -stableaggregates;stability;depth of soil
点击此处可从《中国土壤与肥料》浏览原始摘要信息
点击此处可从《中国土壤与肥料》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号