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SOIL LOSS FROM EROSION IN THE NEXT 50 YEARS IN KARST REGIONS OF MAYABEQUE PROVINCE, CUBA

机译:古巴马雅比​​克喀斯特地区近50年侵蚀造成的土壤流失

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To date, neither the method nor diagnostic indices employed in Cuba to evaluate erosion of Red Ferralitic or Ferrasol Rhodic soil in karstic regions has taken into consideration morphogenesis in such geo-ecosystems or their relationship with erosion, which has led to sequential degradation of the most productive soils in Cuba. We explore the case for considering A+B horizon depth as one of the basic indices for evaluating the severity of erosion. There is no methodology available for estimating the volume of soil lost through karstic absorption forms (dolines). This article forecasts loss of soil cover using a model which estimates losses of 26852 to 45052mmy(-1) for future scenarios (periods of 25 and 50years). A mean loss rate of 107mmy(-1) was found in areas cultivated as pastureland during the period from 1986 to 2009, which exceeds the tolerance thresholds proposed by the Universal Soil Loss Equation and the soil formation rates estimated for limestone in Cuba and it is likely there is with a marked tendency for this to increase. These results should be interpreted as a first estimate for setting loss tolerances as there is no similar experience with own data for a more precise definition of the erosion of soil in karstic regions. Copyright (c) 2012 John Wiley & Sons, Ltd.
机译:迄今为止,古巴用于评估岩溶地区红色铁质或法拉索Rhodic土壤侵蚀的方法和诊断指标都没有考虑到此类地质生态系统中的形态发生及其与侵蚀的关系,这导致了大多数古巴的多产土壤。我们探讨了将A + B视线深度作为评估侵蚀严重程度的基本指标之一的情况。没有方法可用于估算通过岩溶吸收形式((线)流失的土壤量。本文使用一个模型来预测土壤覆盖率的损失,该模型估计未来情况(25年和50年)的损失为26852至45052mmy(-1)。在1986年至2009年期间,在作为牧场的耕地中发现的平均流失率为107mmy(-1),超过了世界土壤流失方程和古巴石灰岩的土壤形成率所估计的容忍度阈值。可能有明显的增加趋势。这些结果应被解释为设定损失容忍度的初步估计,因为对于岩溶地区土壤侵蚀的更精确定义,对于自身数据没有类似的经验。版权所有(c)2012 John Wiley&Sons,Ltd.

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