以横断秦岭-黄淮平原交界带中部的土壤断面为研究对象，应用土壤地球化学观点，讨论了交界带土壤物质迁移和积累规律。
The studied object in this paper is the soil section from west to east that acrosses the middle juncture of Qinling-Huanghuai.
除离海岸线较远的监测断面属轻度土壤盐渍化外，其他监测断面均为重度土壤盐渍化。
Monitoring sections farther away from the shoreline was mild soil salinization, other monitoring sections was severe soil salinization.
并基于达西定律探讨了断面平均土壤含水率与纵向距离之间的关系。
Relationships between average soil moisture content and vertical distance were discussed based on the Darcy"s law."
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