摘要
针对莱州湾南岸重盐渍化土地复垦利用过程中存在的土壤盐碱、瘠薄等障碍问题,选择重盐渍化区的典型地块作为研究对象,运用地统计学和GIS技术,研究不同土壤盐分离子的空间变异性及其相关关系,并绘制各盐分离子的空间分布图。结果表明:不同深度的土壤盐分离子质量浓度变幅差异较大,最大达到124.34mg·L(-1);各土壤盐分离子质量浓度随着土壤深度的增加而增加,变异系数为10%~100%,属于中等强度变异。偏相关分析结果表明各盐分离子间的相关关系复杂;聚类分析将各盐分离子分为3类:第一类包括TS,σ,TDS,SO_4^(2-),Mg^(2+),K^+,Na^+,Cl^-和Ca^(2+),第二类包括SAR和Cl^-/SO_4^(2-)比值,第三类主要是NO_3^-。各盐分离子的块基比均小于25%,具有强烈的空间相关性,表明盐分离子的空间分布主要受结构性因素影响;空间自相关距离为87.88~215.57m,均大于取样间距40m。克里格(Kriging)插值结果表明:研究区土壤含盐量呈明显的带状分布,土壤含盐量从东北部往西南部逐渐增加,东南部土壤含盐量最高;研究区土壤碱化程度较低,盐渍化类型主要为硫酸盐型。该研究为莱州湾南岸重盐渍化区盐渍土的分区、改良、管理和合理利用提供了理论基础和参考依据。
The southern coastal area of the Laizhou Bay has been one of the most severest area affected by soil salinization.In view of the obstacle problems(e.g.,soil salinization,poor soil quality,etc)in the reclamation process of the abandoned salt pan,this study selected this severest salinization area as research targeted region,and used geostatistics and GIS technology to study on the spatial variability and the correlativity of different soil salt ions and to visually present the spatial distributional patterns of the salt ions.Results showed that the soil salt ion contents varied greatly at different depths and the maximum value was 124.34 mg·L-1.The content of each salt ion increased with the depth,and the range of the variation coefficient was 10%~100%,which belonged to moderate variation.The partial correlation analysis showed complex correlations among the salt ions.The salt ions can be divided into three categories by cluster analysis.The first category included TS,EC,TDS,SO^2-4,Mg^2+,K^+,Na^+,Cl^-,and Ca^2+,the second category were SAR and Cl-/SO 2-4,and the third category was mainly NO-3.The nugget/sill ratio of all the salt ions was less than 25%,indicating a strong spatially correlation.And,the spatially distribution of salt ions was mainly affected by structural factors.The spatial autocorrelation distances ranged from 87.88 m to 215.57 m,which were all longer than the sampling interval(40 m).As shown by the results of Kriging interpolation,the spatial distribution of soil salinity in the study area took on an apparent strip style,soil salinity increased from northeast to southwest sides,and the highest soil salinity was observed in the southeast side.The degree of soil alkalization was low,and sulfate type was the primary salinization type.This study provides some theoretical basis and references for the partition,amelioration,management and rational utilization of saline soil in the severe salinization regions in the southern coastal area of the Laizhou Bay.
作者
刘文全
卢芳
于洪军
王传珺
徐兴永
付腾飞
陈广泉
LIU Wen-quan;LU Fang;YU Hong-jun;WANG Chuan-jun;XU Xing-yong;FU Teng-fei;CHEN Guang-quan(The First Institute of Oceanography,SOA,Qingdao 266061,China;Key Laboratory of Marine Sedimentology and Environmental Geology,Qingdao 266061,China;Laboratory for Marine Geology,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao 266061,China;Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering,College of Environmental Science and Engineering,Ocean University of China,Qingdao 266100,China;Key Laboratory of Marine Environment&Ecology,Ministry of Education,Qingdao 266100,China;National Deep Sea Center,Qingdao 266200,China;National Marine Environmental Monitoring Center,Dalian 116023,China)
出处
《海洋科学进展》
CAS
CSCD
北大核心
2018年第4期586-596,共11页
Advances in Marine Science
基金
国家自然科学基金委-山东省人民政府海洋科学研究中心联合资助项目--海洋地质过程与环境(U1606401)
中央级公益性科研院所基本科研业务费专项资金资助项目--滨海地区海水入侵和土壤盐渍化"数字化"监测预警系统研究(2015T01)
海洋公益性行业科研专项--海岛生态脆弱性综合评估方法体系研究(2015418012-1)
关键词
莱州湾南岸
废弃盐田
土壤盐分
地统计学
空间变异
the southern coastal area of Laizhou Bay
abandoned salt pan
soil salinity
geostatistics
spatial variation