梅芹芹, 龚绪龙,史雅栋, 等2020.江苏沿海盐渍土盐渍化程度及其影响因素分析[J].工程地质学报, 28(5): 959-965. doi: 10. 13544/j.cnki.jeg.2020-247.
    引用本文: 梅芹芹, 龚绪龙,史雅栋, 等2020.江苏沿海盐渍土盐渍化程度及其影响因素分析[J].工程地质学报, 28(5): 959-965. doi: 10. 13544/j.cnki.jeg.2020-247.
    Mei Qinqin, Gong Xulong, Shi Yadong, et al. 2020. Study on salinization degree and its influential factors of saline soil in coastal area of Jiangsu province[J]. Joumal of Engineering Geology, 28(5): 959-965. doi: 10.13544/j.cnki.jeg.2020-247.
    Citation: Mei Qinqin, Gong Xulong, Shi Yadong, et al. 2020. Study on salinization degree and its influential factors of saline soil in coastal area of Jiangsu province[J]. Joumal of Engineering Geology, 28(5): 959-965. doi: 10.13544/j.cnki.jeg.2020-247.

    江苏沿海盐渍土盐渍化程度及其影响因素分析

    STUDY ON SALINIZATION DEGREE AND ITS INFLUENTIAL FACTORS OF SALINE SOIL IN COASTAL AREA OF JIANGSU PROVINCE

    • 摘要: 盐渍土是江苏沿海地区开发建设需关注的地质环境问题之一。本文系统采集5 m以浅的土样,开展易溶盐试验,研究了江苏沿海盐渍土分布规律、盐渍化程度及影响因素。研究结果表明:全区盐渍土平行于海岸线分布;以中、弱盐渍土为主,强盐渍土零星分布。受沉积环境、气候、水文地质条件、人类活动等共同影响,盐渍化程度空间差异明显。平面上,盐渍化程度呈北强南弱、向海岸线方向延伸有逐渐增强的趋势,强盐渍土分布于连云港黏性土区,岩性、地下水矿化度为主导影响因素。垂向上,表层普遍积盐,连云港地区分带不明显,大丰和南通地区自地表而下可划分为三带,表层土蒸发积盐、中层盐动态变化、下层土饱水盐稳定,地下水位、土体结构为主导影响因素。随着沿海大开发的快速推进,为防止次生盐渍化问题,需关注地面沉降导致的地面高程损失诱发海水入侵加重表层土盐渍化,工程建设中可设置隔离层截断高矿化度地下水的毛细作用。

       

      Abstract: Saline soil is one of the geological environment problems encountered in the construction of project in the coastal area. This paper takes saline soil samples shallower than 5 m depth to test the content of dissolvable salt,and studies the distribution principle,salinization degree and its influential factors of saline soil. The experiment results show that the distribution of saline soil is parallel to the coastline. Medium and weak saline soils take the majority and strong saline soil distributes sporadically. Salinization degree varies greatly under the influences of sedimentary environment,climate,hydrogeological conditions and human activities. In the horizontal direction,salt content and salinization degree are more and more obvious toward the coastal line,and strongly in the north but weakly in the south. Strong saline soil is distributed in the clayed soil area of Lianyungang. Lithology and groundwater mineralization serve as dominant influential factors. In the vertical direction,salt accumulation is common in the surface layer. The zoning in Lianyungang area is not obvious. Dafeng and Nantong districts can be divided into 3 zones from the shallow ground to the deeper layer,with salt accumulation section,changeable salt content section,and salt solution section. Groundwater level and soil layer construction serve as dominant influential factors. With the rapid promotion of grand development of the coastal area,to avoid the secondary salinization,it shall pay attention to the ground elevation loss derived from land subsidence,which would induce seawater intrusion and thus enhance the salinization of topsoil. In the engineering development,it can set isolated layer to cut off the capillarity of underground water with high salinity.

       

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