Xian Lihua, Lu Dehao, Yang Yuantong, Feng Jiayi, Fang Jianbo, Jacobs Douglass F, Wu Daoming, Zeng Shucai
College of Forestry & Landscape Architecture, South China Agricultural University, Guangzhou, China.
Guangdong Eco-Engineering Polytechnic, Guangzhou, Guangdong, China.
Sci Rep. 2024 Jun 12;14(1):13468. doi: 10.1038/s41598-024-64163-9.
Sewage sludge (SS) application to forest plantation soils as a fertilizer and/or soil amendment is increasingly adopted in plantation forest management. However, the potential risks of SS-derived heavy metals (HMs) remain a concern. Many factors, including woodland slope may affect the risks, but the understanding of this issue is limited. This research evaluated the HMs migration via surface runoff, interflow, and sediments when SS was applied in woodlands of varying slopes. We conducted indoor rainfall simulations and natural rainfall experiments to clarify the effect of slope on the migration of HMs via runoff (including surface and interflow) and sediments. In the simulated rainfall experiment, HMs lost via sediments increased by 9.79-27.28% when the slope increased from 5° to 25°. However, in the natural rainfall experiment, when the slope of forested land increased from 7° to 23°, HMs lost via surface runoff increased by 2.38% to 6.13%. These results indciate that the surface runoff water on a high slope (25°) posed high water quality pollution risks. The migration of HMs via surface runoff water or interflow increased as the steepness of the slope increased. The total migration of Cu, Zn, Pb, Ni, Cr and Cd via sediment greatly exceeded that via surface runoff and interflow. Particles ≤ 0.05 mm contributed the most to the ecological risks posed by sediments. Cd was the main source of potential ecological risks in sediments under both experimental conditions.
在人工林经营中,越来越多地采用将污水污泥(SS)作为肥料和/或土壤改良剂施用于人工林土壤的做法。然而,源自SS的重金属(HMs)的潜在风险仍然令人担忧。许多因素,包括林地坡度,可能会影响这些风险,但对这一问题的了解有限。本研究评估了在不同坡度的林地施用SS时,HMs通过地表径流、壤中流和沉积物的迁移情况。我们进行了室内降雨模拟和自然降雨实验,以阐明坡度对HMs通过径流(包括地表径流和壤中流)和沉积物迁移的影响。在模拟降雨实验中,坡度从5°增加到25°时,通过沉积物流失的HMs增加了9.79 - 27.28%。然而,在自然降雨实验中,当林地坡度从7°增加到23°时,通过地表径流流失的HMs增加了2.38%至6.13%。这些结果表明,高坡度(25°)的地表径流水带来了较高的水质污染风险。HMs通过地表径流水或壤中流的迁移随着坡度的增加而增加。Cu、Zn、Pb、Ni、Cr和Cd通过沉积物的总迁移量大大超过了通过地表径流和壤中流的迁移量。粒径≤0.05 mm的颗粒对沉积物造成的生态风险贡献最大。在两种实验条件下,Cd都是沉积物中潜在生态风险的主要来源。