中国农业气象 ›› 2021, Vol. 42 ›› Issue (03): 169-180.doi: 10.3969/j.issn.1000-6362.2021.03.001

• 农业生态环境栏目 •    下一篇

长期免耕旱作对冬小麦生长季土壤剖面有机碳含量的影响

白重九,王健波,董雯怡,刘秀,刘恩科   

  1. 1. 中国农业科学院农业环境与可持续发展研究所,北京 100081;2. 北京市延庆区农业农村局,北京 100142
  • 收稿日期:2020-09-18 出版日期:2021-03-20 发布日期:2021-03-20
  • 通讯作者: 刘恩科,研究员,研究方向为旱地农业,E-mail:liuenke@caas.cn E-mail:liuenke@caas.cn
  • 作者简介:白重九,E-mail: 1208593325@qq.com
  • 基金资助:
    国家自然科学基金国际(地区)合作与交流项目(31961143017);国家自然科学基金面上项目(31470556;31871575);国家自然科学基金青年基金项目(41601328);公益性行业(农业) 科研专项项目(201503120);中国农业科学院生物节水与旱作农业创新团队项目;中国农业科学院农业环境与可持续发展研究所中央级公益性科研院所基本科研业务费专项资金项目

Effects of Long-Term No-Tillage on Soil Organic Carbon Contents of Winter Wheat in Different Soil Layers and Growth Period

BAI Chong-jiu, WANG Jian-bo, DONG Wen-yi, LIU Xiu, LIU En-ke   

  1. 1. Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing 100081, China; 2.Yanqing District Bureau of Agriculture and Rural Affairs of Beijing Municipality, Beijing 100142
  • Received:2020-09-18 Online:2021-03-20 Published:2021-03-20

摘要: 依托21a长期免耕秸秆还田定位试验,探究长期免耕加秸秆还田的田间管理方式对冬小麦生长季0−60cm土层内土壤有机碳(SOC)和土壤活性有机碳(MBC、POC、DOC)的影响。试验共设长期免耕秸秆还田(NT)与常规耕作(CT)两种耕作模式,分析0−60cm土层内土壤总有机碳(SOC)、土壤微生物量碳(MBC)、土壤颗粒有机碳(POC)、土壤可溶性碳(DOC)含量的变化。结果表明,在0−20cm土层,NT处理SOC含量显著高于CT处理,其中0−5cm和5−10cm土层平均SOC含量分别增加了81.2 %和52.9 %,冬小麦不同生育期内土壤SOC含量变化不显著;在0−30cm土层内,与CT处理相比,NT显著改变了土壤MBC、POC及DOC在播种前、越冬前、拔节期、开花期和成熟期5个生育阶段的分布情况,且显著提高了5个生育阶段内土壤活性有机碳的含量(P<0.05),其中0−5cm土层内,土壤MBC、POC及DOC含量在各个时期相较于CT处理分别增长60.8%~161.4%、71.8%~141.1%和21.9%~104.4%。0−60cm土层内,两种耕作方式下的SOC、MBC、POC、DOC均随着土壤深度的增大呈下降趋势。说明长期免耕可提高耕作层土壤有机碳含量和小麦生长季活性有机碳的水平,这为旱地土壤有机碳的高效固存提供了理论依据。

关键词: 土壤有机碳, 土壤活性有机碳, 免耕秸秆还田, 冬小麦, 北方旱地

Abstract: Based on a 21-year long-term no-tillage and straw-returning test, aimed to analyze the effects of long-term no-tillage and straw-returning on soil SOC(Soil organic carbon) and its components in the surface and subsoil(0−60cm) in the winter wheat growing period. This long-term fixed experiment started in 1992,included straw-returning under no-tillage(NT) and conventional tillage(CT), two field management methods. The chemical fertilizer was applied to the two treatment are same. After 20-year later, soil samples in different layers and wheat growth period were collected. Soil organic carbon(SOC), soil microbial biomass carbon(MBC), and soil particulate organic carbon(POC) were measured, soil soluble carbon(DOC) content in different soil layers and growth period. Compared with CT, NT significantly changed the distribution of MBC, POC, and DOC of 0−30cm soil layer in the five growth stages before sowing, before winter, jointing, anthesis, and maturity. Furthermore, NT significantly improved their soil contents in the five stages(P<0.05), specifically, in comparison, MBC, POC, and DOC in the five growth stages increased averagely by 60.8%−161.4%, 71.8%−141.1%, and 21.9%−104.4%, respectively. Besides, there is a great influence on SOC content in the 0−20cm soil layer by applying no-tillage and straw-returning; the average SOC content of 0−5cm and 5−10cm soil increased 81.2% and 52.9%, respectively. However, this similar influence did not appear in the 5-growth period. In the layer of 0−60cm, the contents of SOC, MBC, POC, and DOC under two tillage methods all showed a downward trend with soil depth growth. The organic carbon content of surface soil(0−20cm) and the level of active organic carbon(MBC, POC, DOC) in the wheat-growing time were significantly improved after applying no-tillage and straw-returning. This study showed that long-term no-tillage could raise the soil organic carbon content and active organic carbon level during the wheat growing season, which provides a theoretical basis for the efficient storage of organic carbon in dryland soil.

Key words: Soil organic carbon, Soil labile organic carbon, No-tillage straw returning, Winter wheat, Dryland in the North