首页 | 本学科首页   官方微博 | 高级检索  
     

赤红壤旱地土壤有机质的消长规律
引用本文:方玲,高志强,姚宝全,罗光,林依汝. 赤红壤旱地土壤有机质的消长规律[J]. 福建农林大学学报(自然科学版), 1992, 0(4)
作者姓名:方玲  高志强  姚宝全  罗光  林依汝
作者单位:福建农学院土壤农化系,福建农学院土壤农化系,龙岩市环保局,福建农学院土壤农化系,福建农学院土壤农化系 福州 350002,福州 350002,龙岩 364000,福州 350002,福州 350002
摘    要:采用不同的输套作制度及其所产生的稿秆、绿肥等回田并配合施用无机肥料的培肥管理措施,在莆田沿海赤红壤旱地进行两年的小区和示范片的试验,结果表明:两年来土壤有机质增加0.07%—0.38%,全氮含量增加0.01%—0.05%,有机物质的年分解率达38%—76%,有机物质的腐殖化系数为0.1—0.25,土壤有机质的氧化稳定度保持在0.52—0.69。这说明土壤自身的物质和能量已逐渐进入良性的交换循环中,预计按此模式进行培育土壤有机质,在今后的一二十年内土壤有机质可达到2%左右。

关 键 词:赤红壤旱地土壤  土壤有机质  年分解率  腐殖化系数  氧化稳定度

The Rising and Failing Regularity of Organic Matter in Lateritic Red Soil
Fang Ling Gao Zhiqiang Yao Baoquang Luo Guang Lin Yilu. The Rising and Failing Regularity of Organic Matter in Lateritic Red Soil[J]. Journal of Fujian Agricultural and Forestry University, 1992, 0(4)
Authors:Fang Ling Gao Zhiqiang Yao Baoquang Luo Guang Lin Yilu
Affiliation:Fang Ling~1 Gao Zhiqiang~1 Yao Baoquang~2 Luo Guang Lin Yilu~1
Abstract:Through the experiments applied the straw and legume crops produced by the different systems of rotation and relay of crops, and applied in company with the inorganic fertilizer, the contents of soil organic matter increased 0.07-0.38% and the nitrogen content increased 0.01—0.05% after two years.The decompound percentage of organic substances was kept an average of 38-76% a year.The humification coefficient of organic substances was 0.1—0.25.The oxidution stability coefficient of soil organic matter was kept up 0.52—0.69.According to this fertilizing, the contents of soil organic matter would increase from 0.86% to 2% in ten or twenty years.
Keywords:lateritic red matter  soil organic matter  decompound percentage in a year  humification coefficient  osidution stability coefficient
本文献已被 CNKI 等数据库收录!
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