为了消减盐碱障碍和提升地力,研究了苏北典型滩涂新垦农田土壤盐分的空间变异性。结果表明,农田土壤盐分东低西高,整体上属轻度盐渍化(含盐量1.27~1.98g/kg),但存在着盐斑(含盐量大于2g/kg)。表层及次表层土壤含盐量空间自相关程度强烈,其结构方差比分别为88.88%、80.75%;而其余土层含盐量间自相关程度为中等。垂直方向上,土壤盐分主要集中在犁底层(20~40cm)。
The spatial variability of saline-alkaline was studied to reduce soil salt content and inprove land fertility in the reclaimed mudflat farmland. The results showed that field was mild salinization with some por- phyritic severe salinization in the southwest. The spatial heterogeneity degrees of 0~20 crn and 20~40 cm in soil depth were strong dependent with the structural variation ratio [C/(C+Co)] of 88.88%, 80.75% respec- tively however, only moderate degree of spatial heterogeneity was found in the other three soil layers. The top of soil salt content appeared in the 20~40 cm soil layer, which was the plow pan of the study field.