荷兰土地利用变化对净固碳的影响

J. Wolf, Larry Janssen
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引用次数: 19

摘要

本文确定了荷兰耕地、草地和森林三种土地利用系统的平均碳流和碳库。对于收获的产品,统计数据是有用的,它们被用作计算碳流量的基础。平均碳库,特别是土壤中的碳库,不能直接得到。为了计算这个碳库,采用了一种只需要三个输入数据的方法:作物或树木残留物的平均数量,土壤有机质的分解率和所谓的腐殖质系数。对于广泛的研究,这种简单的方法特别有用。然而,这种方法只能适用于平衡的情况,即作物残茬或凋落物的掺入率与土壤有机质的分解率刚好相等,因此土壤碳是恒定的。在土壤中,由于作物轮作和土地利用的不断变化,平衡状态可能不会真正发生。对于不断变化的土地利用以及由此产生的有机物质掺入率的变化,展示了如何计算新的平衡状态和碳库大小的变化率。对于荷兰土地利用的一些实际变化,确定了碳库大小的变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of changing land use in the Netherlands on net carbon fixation
For three land use systems, arable land, grassland and forest, average carbon flows and car­ bon pools in the Netherlands have been determined. For harvested products data are avail­ able from statistics and they were used as a basis for calculating the carbon flows. Average carbon pools, particularly in the soil, cannot be derived directly. For the calculation of this carbon pool a method has been applied that requires only three input data: the average amount of crop or tree residues, the decomposition rate of soil organic matter and the so­ called humification coefficient. For broad studies this simple method can particularly be use­ ful. However, this method can only be applied to situations in equilibrium, where the rates of incorporation of crop residues or tree litter and decomposition of soil organic matter are just equal and hence, the soil carbon is constant. In the soil, a state of equilibrium may not really occur, as continually changes in crop rotation and land use will take place. For a changing land use and hence a changing rate of incorporation of organic material it is shown how the new state of equilibrium and the rate of change in carbon pool size can be calculated. For a number of actual changes in land use in the Netherlands the resulting changes in carbon pool sizes were determined.
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