Jordán-López Antonio, Martínez-Zavala Lorena, Bellinfante Nicolás
MEDSoil Research Group, Dpto. de Cristalografía, Mineralogía y Química Agrícola, Facultad de Química (Universidad de Sevilla), Sevilla, Spain.
Sci Total Environ. 2009 Jan 1;407(2):937-44. doi: 10.1016/j.scitotenv.2008.09.047. Epub 2008 Nov 7.
Surface runoff and sediment production on unpaved forest roads in a humid Mediterranean mountainous area has been studied using a simple portable rainfall simulator at an intensity of 90 mm h(-1). Thirty six rainfall simulations were carried out on road plots: on the roadbank (12), on the sidecast fill (12), and on the roadbed (12). On the roadbanks, the steady-state runoff coefficient was 85.9% and runoff flow appeared after 63 s on average. On the sidecast fills, the steady-state runoff coefficient was 58.6% and mean time to runoff was 48 s. Finally, on the roadbeds, the steady-state runoff coefficient was 21.5% and mean time to runoff was 41 s. The highest soil loss rate was found on the roadbanks (486.7 g m(-2)), mainly due to low plant cover, soil texture and rock fragments. The total soil erosion on the roadbanks was 3 and 18 times higher than those from the roadbeds and the sidecast fills, respectively. As a consequence, roadbanks can be considered the main source of sediments on the studied sites, but the function of unpaved forest roads as source points for runoff generation is more important.
在湿润的地中海山区,使用一台强度为90毫米/小时的简易便携式降雨模拟器,对未铺砌的林道上的地表径流和产沙情况进行了研究。在道路地块上进行了36次降雨模拟:在路肩(12次)、弃土堆填方(12次)和路基(12次)上。在路肩上,稳态径流系数为85.9%,平均63秒后出现径流。在弃土堆填方上,稳态径流系数为58.6%,径流平均出现时间为48秒。最后,在路基上,稳态径流系数为21.5%,径流平均出现时间为41秒。路肩上的土壤流失率最高(486.7克/平方米),主要原因是植被覆盖度低、土壤质地和岩石碎片。路肩上的总土壤侵蚀量分别比路基和弃土堆填方高3倍和18倍。因此,路肩可被视为研究地点沉积物的主要来源,但未铺砌的林道作为径流产生源点的作用更为重要。