摘要
应用土壤电导率与基模吸力的关系,判断和测定了土壤的进气值,采用改进后的砂型漏斗装置测定了土壤的发泡点。对脱水过程中3个不同剖面层次土壤进气值和发泡点的测定结果表明,耕作表层(A p)土壤的进气值和发泡点分别为1.343和5.880 kPa;淋溶淀积过渡层(AB)土壤的进气值和发泡点分别为2.597和4.116kPa;埋藏表层(A b)土壤的进气值和发泡点分别为0.451和6.076 kPa。由此可见,土壤的进气值与发泡点的数值明显不同,进气值与发泡点是2个不同的概念。
Relationship between soil electric conductivity and soil matric suction was used to estimate soil air entry value. Sand mold funnel apparatus provided in this paper was identified as the method for the measurement of soil bubbling point. Air entry value and bubbling point of three profile layers during desorption were measured:Air entry value of Ap horizon was 1. 343 kPa,the bubbling point 5. 880 kPa. Air entry value and bubbling point of AB horizon were 2. 597 kPa and 4. 116 kPa respectively. Air entry value and bubbling point of Ab horizon were 0. 451 kPa and 6. 076 kPa respectively. The measured results show that the air entry value and bubbling point are two concepts with different values.
出处
《西北农林科技大学学报(自然科学版)》
CSCD
北大核心
2005年第9期108-112,共5页
Journal of Northwest A&F University(Natural Science Edition)
基金
国家自然科学基金项目(5020900150479064)
北京市科技新星计划项目(H020821340130)
关键词
土壤
进气值
发泡点
电导率
基模吸力
soil
air entry value
bubbling point
electric conductivity
matric suction