封丘县土壤障碍因子探析  

Analysis on Soil Obstacle Factors in Fengqiu County

作　　者：李开丽[1] 檀满枝[2] 孙汉群[1] LI Kaili;TAN Manzhi;SUN Hanqun(College of Geosciences,Jiangsu Second Normal University,Nanjing Jiangsu 210013;Institute of Soil Science,Chinese Academy of Sciences,Nanjing Jiangsu 210008)

机构地区：[1]江苏第二师范学院地理科学学院,江苏南京210013 [2]中国科学院南京土壤研究所,江苏南京210008

出　　处：《现代农业科技》2023年第6期155-159,共5页Modern Agricultural Science and Technology

基　　金：中国科学院知识创新工程重大项目(KSCX1-YW-09-02)。

摘　　要：本文基于1981年土壤普查数据,2008年、2009年测产数据,测产点土壤盐分数据及2008年地下水最大埋深数据,分析了土壤剖面质地构型、盐分及地下水因子对作物产量的影响。结果表明,底沙漏沙型和盐层型土壤不属于障碍类型,其中底沙漏沙型土壤产量最高,盐层型土壤部分年份超过了无障碍土壤。测产数据与地下水及盐分的相关分析表明,盐分仍然是限制性因子,仍需防范土壤次生盐渍化。Based on the soil census data in 1981,the production measurement data in 2008 and 2009,the soilsalinity data at the production point and the maximum groundwater depth data in 2008,this paper analyzed the impact ofsoil profile texture,salinity and groundwater factors on crop yield.The results showed that the bottom sand sand leakagetype soil and the salt layer type soil were not obstacle types,and the yield of bottom sand sand leakage type soil was thehighest,the salt layer type soil exceeded the barrier-free soil in some years.The correlation analysis between theproduction measurement data and groundwater and soil salinity showed that salinity was still a limiting factor,andsecondary salinization of soil still needed to be prevented.

关 键 词：地下水 土壤盐分 土壤剖面质地构型 障碍因子 作物产量 河南封丘 

分 类 号：S152.2[农业科学—土壤学] S152.3[农业科学—农业基础科学] S156.1