首页 | 本学科首页   官方微博 | 高级检索  
     检索      

土壤结构改良剂对皖南旱地红壤水分特征的影响
引用本文:潘金华,庄舜尧,史学正,曹志洪,蔡宪杰,程森.土壤结构改良剂对皖南旱地红壤水分特征的影响[J].水土保持通报,2016,36(5):40-45.
作者姓名:潘金华  庄舜尧  史学正  曹志洪  蔡宪杰  程森
作者单位:1. 中国科学院南京土壤研究所,土壤与农业可持续利用国家重点实验室,江苏南京210008;2. 上海烟草集团责任有限公司,上海,200082
基金项目:沪皖现代烟草农业高科技示范园科技专项“皖南烟稻优质高效生态安全的土肥综合技术研究与示范”(CF56-ZJ1)
摘    要:目的]研究土壤结构改良剂对皖南旱地红壤孔隙、容重及水分特征的影响,为皖南旱地红壤改良、提高土壤持水保水与抗旱保墒性能提供依据。方法]采用硅藻土(通气性Si改良剂)、泡沫沙类改良剂(T20)和无机矿石类改良剂(G20)等3种土壤结构改良剂,设置1%,2%,5%与10%的4个添加比例,进行土壤物理性状与水分特征测试。结果]硅藻土与T20均可显著降低土壤容重,而G20在添加5%与10%时才显著降低;硅藻土处理土壤毛管孔隙度由52.1%增加到91.3%,优于T20和G20;硅藻土与T20的吸湿系数与凋萎湿度随用量呈先增加而后下降,而G20则随添加量增加而增加;土壤的饱和持水量与田间持水量均随土壤结构改良剂添加量的增加而增加,以硅藻土增加最多,T20次之,G20最少。随改良剂用量增加,土壤有效水及难效水均呈增加趋势,其中,硅藻土处理的难效水增加量显著高于T20与G20处理。结论]改良皖南旱地土壤水分需要根据改良剂材料的种类与用量来进行合理施加,必要时可以组合搭配使用,从而达到最优效果。

关 键 词:土壤结构改良剂  皖南旱地  土壤容重  孔隙度  土壤水分
收稿时间:2015/12/11 0:00:00
修稿时间:7/8/2016 12:00:00 AM

Effects of Soil Amendments on Water Characteristics in Red Soil of Upland in South Anhui Province
PAN Jinhu,ZHUANG Shunyao,SHI Xuezheng,CAO Zhihong,CAI Xianjie and CHENG Sen.Effects of Soil Amendments on Water Characteristics in Red Soil of Upland in South Anhui Province[J].Bulletin of Soil and Water Conservation,2016,36(5):40-45.
Authors:PAN Jinhu  ZHUANG Shunyao  SHI Xuezheng  CAO Zhihong  CAI Xianjie and CHENG Sen
Institution:State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China,State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China,State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China,State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, Jiangsu 210008, China,Shanghai Tobacco Group Limited Company, Shanghai 200082, China and Shanghai Tobacco Group Limited Company, Shanghai 200082, China
Abstract:Objective] The aim of this study is to investigate the effects of soil amendments on soil porosity, bulk density and water characteristics of upland at South Anhui Province, in order to provide information for soil improvement, water availability and anti-drought.Methods] Three different kinds of soil amendments including diatomite(Si), foamed sand(T20) and mineral amendment(G20) were used and 4 addition rates of 1%, 2%, 5% and 10% were adopted in the batch experiment.Results] The addition of Si and T20 reduced soil bulk density significantly, however, the addition of G20 showed a significant effect only at the addition rate of 5% and 10%. Soil porosity increased from 52.1% to 91.3% by Si treatment, which was better than T20 and G20 treatment. Soil moisture absorption coefficient and wilting moisture increased first and then decreased with the application amount of Si and T20. In contrast, soil moisture absorption coefficient and wilting moisture increased linearly with the application amount of G20. Soil saturation water capacity and field water capacity increased with the application amount of three amendments, and the increase trend was largest by application of Si, followed by T20 and G20. In addition, soil available water and hard available water increased with soil amendment addition rate. The treatment of Si on hard available water was better than T20 and G20.Conclusion] The water characteristics of upland soil of South Anhui Province should be improved according to the type and amount of soil amendment. In order to achieve an ideal effect, the combination of various soil amendments should be taken into account.
Keywords:soil amendment  South Anhui Province upland  soil bulk density  soil porosity  soil water
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《水土保持通报》浏览原始摘要信息
点击此处可从《水土保持通报》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