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Land use changes and soil redistribution estimation using Cs-137 in the tropical Bera Lake catchment, Malaysia

机译:利用Cs-137在马来西亚热带贝拉湖流域进行土地利用变化和土壤再分配估计

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The catchment of Bera Lake in Pahang State, Peninsular Malaysia has experienced severe land use changes since 1972 with some 340 km(2) (out of a total area of similar to 600 km(2)) having been converted to oil palm and rubber plantations and in some places, newly cleared for monoculture. The proportional model using the Cs-137 radionuclide was recognized as being the most suitable conversion model for estimating soil redistribution in the catchment as the deforested land has been cultivated once in a medium-term range of 30-40 years. Thirty-five bulk core soil samples were taken to a depth of 25 cm in areas of different land use and known dates of tillage commencement in the catchment. Ten bulk core samples were also collected in the bottom sediments of wetlands and open waters to estimate accumulation rates in these sink areas. Individual land development districts with known elapsed times from start of tillage allowed determination of soil redistribution rates and preparation of a soil redistribution map. A mean soil erosion rate of 915 +/- 345 t h(-1) y(-1) was determined in areas of cleared land, whereas rates of 117 +/- 36, and 70 +/- 35 t h(-1) y(-1), were determined in areas of developing, and developed, oil palm and rubber plantations, respectively. The overall accumulation rate of eroded soils within the wetlands and open waters was determined to be 1.025 cm y(-1) since 1995. The Bera Lake catchment soil redistribution map is the first attempt in Malaysia to map soil redistribution using the Cs-137 technique on a catchment scale. The soil redistribution map will provide good guidelines for future soil conservation practices and sustainable land use programs. (C) 2013 Elsevier B.V. All rights reserved.
机译:自1972年以来,马来西亚半岛彭亨州贝拉湖流域经历了严重的土地利用变化,大约340 km(2)(总面积接近600 km(2))已转变为油棕和橡胶种植园在某些地方,新近可以进行单一栽培。使用Cs-137放射性核素的比例模型被认为是估计流域土壤再分配的最合适的转换模型,因为砍伐的土地在30至40年的中期范围内已耕种过一次。在不同土地用途和集水区耕作开始的已知日期,将25个散装芯土壤样品采集到25厘米深处。在湿地和开放水域的底部沉积物中还收集了十个散装岩心样品,以估计在这些汇区的积累率。从耕作开始到经过的时间已知的各个土地开发区,可以确定土壤的重新分配速率并准备土壤重新分配图。在开垦土地上确定的平均土壤侵蚀率为915 +/- 345 th(-1)y(-1),而土壤侵蚀率为117 +/- 36和70 +/- 35 th(-1)y (-1)分别在开发中和开发中的油棕和橡胶园确定。自1995年以来,湿地和开阔水域中侵蚀土壤的总体累积速率确定为1.025 cm y(-1)。贝拉湖流域土壤重新分布图是马来西亚首次尝试使用Cs-137技术绘制土壤重新分布图在集水规模上。土壤再分配图将为未来的土壤保护实践和可持续土地利用计划提供良好的指导。 (C)2013 Elsevier B.V.保留所有权利。

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