苟富刚, 陆徐荣, 龚绪龙, 等. 2023. 连云港滨海地区沉积物含盐特征及其对工程基础的影响[J]. 工程地质学报, 31(6): 2071-2081. doi: 10.13544/j.cnki.jeg.2021-0448.
    引用本文: 苟富刚, 陆徐荣, 龚绪龙, 等. 2023. 连云港滨海地区沉积物含盐特征及其对工程基础的影响[J]. 工程地质学报, 31(6): 2071-2081. doi: 10.13544/j.cnki.jeg.2021-0448.
    Gou Fugang, Lu Xurong, Gong Xulong, et al. 2023. Salt characteristics and its impact on engineering foundation soil in Lianyungang marina area[J]. Journal of Engineering Geology, 31(6): 2071-2081. doi: 10.13544/j.cnki.jeg.2021-0448.
    Citation: Gou Fugang, Lu Xurong, Gong Xulong, et al. 2023. Salt characteristics and its impact on engineering foundation soil in Lianyungang marina area[J]. Journal of Engineering Geology, 31(6): 2071-2081. doi: 10.13544/j.cnki.jeg.2021-0448.

    连云港滨海地区沉积物含盐特征及其对工程基础的影响

    SALT CHARACTERISTICS AND ITS IMPACT ON ENGINEERING FOUNDATION SOIL IN LIANYUNGANG MARINA AREA

    • 摘要: 土体含盐特征是环境演化、工程地基基础设计和城市绿地建设的重要参考指标。通过采集连云港滨海地区土样616件,根据测试结果以及土层划分结果对研究区80m以浅土层含盐特征进行了系统分析。研究结果表明:80m以浅土层盐分主要受3次海侵控制,盐分以NaCl为主,其中Cl-含量占比最高达到了62.01%,NaCl含量占比最高达到了94.25%。各土层含盐量介于0.020% ~7.149%。全新世土层含盐量高,以中盐渍土为主。随着深度的增加,土体含盐量有着递减的趋势。含盐量最高土层出现在2-1层黏土中。更新世土层含盐量较高,除了8-2砂层外,均有弱盐渍土出现。受海侵影响,海相土层含盐量均高于其上覆和下伏土层。海侵对下伏地层具有侵染作用,使得陆相地层含盐量增加。同一层组的土层细粒土含盐量一般大于砂土。各土层ESR(交换性钠)值较高,均大于当地地表淡水SAR(钠吸附比)。ESR最大值103出现在3-1软土层,为当地地表淡水ESR值的32倍。各土层统计平均值γMg/γCa范围值为0.80~2.67,均大于当地地表淡水的γMg/γCa值,说明各土层不同程度受到海水入侵的影响。各层土γMg/γCa最大值出现在3-1软土层,说明该层土沉积受控于海侵。各层土pH值均大于7.7,浅部2-1层与3-1层pH值高,土体改良需施加酸性或者钙质改良剂。各土层易溶盐的腐蚀性主要表现在Cl-对混凝土结构中钢筋的腐蚀性,强腐蚀土层主要分布在25m以浅土层,对应土层为3-1层软土和2-1层黏土。给出了土体中Cl-对混凝土结构中钢筋的腐蚀性界限含盐量,工程建设中应注意基础防腐工作。

       

      Abstract: Soil-containing salt characteristics is an important reference indicators for environmental evolution, engineering foundation design and urban green space construction. By collecting 616 earthy samples in Lianyungang, the study is based on the test results and the soil layer division results. The research zone of depth 80m is systematically analyzed by the brine-containing characteristics of the soil layer. The results show that the 80m thick soil is mainly subject to 3 sea assays in the light soil layer. The salt is mainly NaCl, with the highest ratio of Cl- reached 62.01%. NaCl content ratio reaches 94.25%. The containing salt is 0.020% to 7.149%. The new land layer is high salt, and mainly salted soil. As the depth increases, the amount of soil salt contains salt has a declining trend. The highest soil layer containing salt is in 2-1 layer clay. Update the content of the land of the world is high, and there are weak saline soils except for the 8-2 sand layer. Affected by the sea, the salt contained in the sea is higher than that of its overlap and underlap layers. The sea assault has infected infection, so that the amount of the land formation is increased. The soil layer of fine grain soil is generally greater than sand in the same layer. Earth layer ESR value is higher, both greater than local surface freshwater SAR. The ESR maximum 103 appears in the 3-1 soft soil layer, and it is 32 times the ESR value of the local surface fresh water ESR value. The statistical average γMg/γCa range is 0.80~2.67. The γMg/γCa value of soil is larger than the γMg/γCa value of fresh water in the study area, which indicating that the earth layer of the study area is affected by seawater invasion. The largest level of soil γMg/γCa appeared at 3-1 soft soil, which indicating that the layer of soil is controlled by the sea. The pH of each layer is greater than 7.7, and the pH of the light surface layer 2-1 and the 3-1 layer are both 8.3. The soil improvement needs to be applied to an acidic or calcium improvement agent. The corrosion resistance of each soil layer is mainly based on the Cl-corrosiveness of the reinforcement in the concrete structure. The strong corrosive etching layer is mainly distributed at 25m to the soil layer, and the soil layer is 3-1 layer soft soil and 2-1 floors. While giving the corrosive boundary volume of the steel bib in the concrete structure in the soil, the engineering construction should pay attention to the basic anti-corrosion.

       

    /

    返回文章
    返回