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Characterization of soil salinization in typical estuarine area of the Jiaozhou Bay, China

机译:胶州湾典型河口地区土壤盐渍化的特征

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In this study, the characteristics of soil salinization and the effects of main land use/land cover and other factors in typical estuarine area of the Jiaozhou Bay are investigated. Soil samples were collected in the parallel coastal zone, vertical coastal zone and longitudinal profile depth in the area to determine the soil salt content. The correlation analysis and principal component analysis are used to address the general characteristics of soil salinization in the study area. In the horizontal direction, there are moderate salinization, severe salinization and saline soil state. The farther from the sea (within 1.1 km), the lower the soil salinization degree. In the direction of longitudinal profile depth, there are severe salinization and saline soil state, and the soil salt content is accumulated in the surface and bottom. The Na+ and Cl- are the dominant cation and anion, respectively, the distributions of which are consistent with that of salt content. All the salinization indexes, except for soil pH, are of moderate/strong variability. The invasion of Spartina alterniflora results in the increase of soil salt content and salinization degree, the effects of which are mainly determined by the physiological characteristics and the growth years. The degree of soil salinization increased significantly in the aquaculture ponds, which is mainly caused by the use of chemicals. The correlation between soil salt content and Na+, Cl- is particularly significant. From the results of principal component analysis, Na+, Cl-, Ca2+, Mg2+ and SO42- could be used as main diagnostic factors for salinization in typical estuarine area of the Jiaozhou Bay. The effects of NaCl and sulfate on salt content further affect the degree of salinization in the estuarine area. (C) 2017 Elsevier Ltd. All rights reserved.
机译:在这项研究中,研究了土壤盐渍化的特点和主要土地使用/陆地覆盖的影响以及胶州湾典型河口地区的其他因素。在该地区的平行沿海区,垂直沿海区和纵向轮廓深度中收集土壤样品以确定土壤盐含量。相关分析和主成分分析用于解决研究区土壤盐渍化的一般特征。在水平方向上,存在中等的盐渍化,重度盐渍化和盐水土壤状态。越远离海(1.1公里内),土壤盐渍化程度越低。在纵向曲线深度的方向上,存在严重的盐渍化和盐水状态,土壤盐含量累积在表面和底部。 Na +和Cl-分别是阳离子和阴离子,其分布与盐含量一致。除土壤pH外,所有盐渍化指数都具有中等/强烈的可变性。 Spartina Interfiflora的侵袭导致土壤盐含量和盐渍化程度的增加,其效果主要由生理特征和生长年份决定。水产养殖池的土壤盐渍化程度显着增加,主要由化学品造成的。土壤盐含量与Na +,Cl-之间的相关性特别显着。从主成分分析的结果,Na +,Cl-,Ca2 +,Mg2 +和SO42-可以用作胶州湾典型河口地区盐渍化的主要诊断因素。 NaCl和硫酸盐对盐含量的影响进一步影响了偏毒素区域的盐化程度。 (c)2017 Elsevier Ltd.保留所有权利。

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