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Lateral heterogeneity of soil physicochemical properties in riparian zones after agricultural abandonment

机译:弃耕后河岸带土壤理化性质的横向异质性

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摘要

The study aimed to identify the lateral heterogeneity of soil physicochemical properties in riparian zones, and its underlying drivers during natural restoration after agricultural abandonment. Abandoned farmlands, after 5-year natural restoration, within 500 m from the edges on both sides of Liaohe River were selected as the study area. Soil physicochemical properties of four lateral buffers (<10 m, 10~100 m, 100~300 m, and >300 m from river edge, respectively) along riparian zones were measured. The results showed that riparian soils were characterized by high sand content (78.88%~96.52%) and poor soil nutrients. Soil silt content, organic carbon (OC), cation exchange capacity (CEC), total nitrogen (TN), and available nitrogen (AN) increased laterally with increasing distance from river edge, while soil sand content decreased. Total phosphorus (TP) and available phosphorus (AP) are not spatially autocorrelated. Soil OC, TN, AN, and CEC along upstream and midstream reaches showed negative spatial autocorrelation along the lateral gradients, and positive along downstream reach. Altitude, distance from river edge and distance from nearest farmland were the pronounced factors affecting soil physicochemical properties in this study.
机译:该研究旨在确定河岸带土壤理化性质的横向异质性及其在农业废弃后自然恢复过程中的潜在动因。经过5年的自然恢复,距离辽河两岸500 m以内的废弃农田被选为研究区域。测量了沿河岸带的四个侧向缓冲带(分别距河边<10 m,10〜100 m,100〜300 m和> 300 m)的土壤理化性质。结果表明,河岸带土壤含沙量高(78.88%〜96.52%),土壤养分含量低。随着距河边距离的增加,土壤泥沙含量,有机碳(OC),阳离子交换容量(CEC),总氮(TN)和有效氮(AN)横向增加,而土壤含沙量减少。总磷(TP)和有效磷(AP)在空间上不是自相关的。上游和中游河段的土壤OC,TN,AN和CEC沿横向梯度显示为负空间自相关,而下游河段则为正。海拔,距河边缘的距离和距最近农田的距离是影响土壤理化性质的显着因素。

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