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黄土高原旱地不同种植系统对土壤水稳性团聚体及碳氮分布的影响
引用本文:魏艳春,马天娥,魏孝荣,王昌钊,郝明德,张萌.黄土高原旱地不同种植系统对土壤水稳性团聚体及碳氮分布的影响[J].农业环境科学学报,2016,35(2):305-313.
作者姓名:魏艳春  马天娥  魏孝荣  王昌钊  郝明德  张萌
作者单位:1. 西北农林科技大学资源环境学院,陕西 杨凌,712100;2. 西北农林科技大学资源环境学院,陕西 杨凌 712100; 西北农林科技大学黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西 杨凌 712100;3. 陕西出入境检验检疫局技术中心,西安,710068
基金项目:国家自然科学基金项目(41271315,41571296);教育部新世纪优秀人才支持计划(NCET-13-0487);西北农林科技大学优秀青年人才科研专项(2014YQ007)
摘    要:以黄土高原连续进行了27年的长期定位试验为对象,研究了粮-草长周期轮作、粮-豆短周期轮作、玉米连作和小麦连作系统土壤团聚体及其碳氮分布特征,并分析了土壤碳氮分布与土壤团聚体及其碳氮含量之间的关系。结果表明:黄土高原旱作农田土壤中0.053 mm团聚体含量最高,占土壤质量的35%,长周期轮作系统0~20 cm和20~40 cm土层土壤0.25~2 mm团聚体含量高于玉米连作、小麦连作和短周期轮作系统,而0.053 mm团聚体含量低于这3种轮作系统,且长周期轮作系统土壤团聚体的平均重量直径和几何平均直径也较高。种植系统对团聚体有机碳和全氮分布的影响主要体现在0~20 cm土层土壤,长周期轮作系统土壤中2 mm和0.25~2 mm团聚体有机碳含量显著高于其他种植系统,0.25 mm团聚体有机碳含量与其他种植系统差异不显著。长周期轮作系统团聚体全氮含量均显著高于其他种植系统,碳氮比则呈现出相反的趋势。土壤总有机碳、氮含量与团聚体有机碳、氮含量呈极显著正相关关系。土壤有机碳和全氮含量的变化主要取决于0.25~2 mm和0.053~0.25 mm团聚体有机碳和全氮的变化,而且有豆科植物苜蓿长期参与的长周期轮作系统可以有效改善土壤结构,提高土壤和团聚体的有机碳和全氮含量。

关 键 词:黄土高原  旱作农田  种植系统  水稳性团聚体  有机碳  全氮
收稿时间:2015/9/11 0:00:00

Effects of cropping systems on distribution of water-stable aggregates and organic carbon and nitrogen in soils in semiarid farmland of the Loess Plateau
WEI Yan-chun,MA Tian-e,WEI Xiao-rong,WANG Chang-zhao,HAO Ming-de and ZHANG Meng.Effects of cropping systems on distribution of water-stable aggregates and organic carbon and nitrogen in soils in semiarid farmland of the Loess Plateau[J].Journal of Agro-Environment Science( J. Agro-Environ. Sci.),2016,35(2):305-313.
Authors:WEI Yan-chun  MA Tian-e  WEI Xiao-rong  WANG Chang-zhao  HAO Ming-de and ZHANG Meng
Institution:College of Resources and Environment, Northwest A & F University, Yangling 712100, China,College of Resources and Environment, Northwest A & F University, Yangling 712100, China,College of Resources and Environment, Northwest A & F University, Yangling 712100, China;State Key Laboratory of Soil Erosion and Dry Land Farming on the Loess Plateau, Northwest A & F University, Yangling 712100, China,Shaanxi Entry-Exit Inspection and Quarantine Bureau, Xi'an 710068, China,College of Resources and Environment, Northwest A & F University, Yangling 712100, China and College of Resources and Environment, Northwest A & F University, Yangling 712100, China
Abstract:In this paper, we examined the distribution of water stable aggregates and organic carbon(OC) and nitrogen(N) in soils under different cropping systems, using a 27-year field experiment in the Loess Plateau. The relationships between OC and N contents in bulk soil and aggregates were also analyzed. Results showed that <0.053 mm aggregates, accounting for 35%, dominated the soil mass in 0~20 and 20~40 cm soil layers in the semiarid farmland of the Loess Plateau. The percentage of 0.25~2 mm aggregates was higher, but that of <0.053 mm aggregates was lower in the grass-grain rotation system than the other cropping systems. In the grass-grain rotation system, mean weight diameter and geometrical mean diameter of soil aggregates were also greater. The significant effects of cropping system on OC and N associated with aggregates mainly occurred in 0~20 cm layer. The OC content in >2 mm and 0.25~2 mm aggregates was significantly higher in grass-grain rotation system than in the other systems, while OC content in 0.053~0.25 mm and <0.053 mm aggregates did not differ among different cropping systems. The grass-grain system showed higher N content and lower C/N ratio in each aggregate compared with other systems. The OC and N content in bulk soils was positively correlated with OC and N content associated with aggregates. These results suggest that the responses of OC and N in the bulk soil to cropping systems mainly depend on OC and N associated with 0.25~2 mm and 0.053~0.25 mm aggregates. Additionally, grass-grain rotation system has greater potential to improve soil structure and increase the content of OC and N associated with aggregates.
Keywords:Loess Plateau  semiarid farmland  cropping system  water-stable aggregates  organic carbon  total nitrogen
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