首页> 外文期刊>Geoderma: An International Journal of Soil Science >Stable isotopes for characterisation of trends in soil carbon following deforestation and land use change in the highlands of Madagascar
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Stable isotopes for characterisation of trends in soil carbon following deforestation and land use change in the highlands of Madagascar

机译:稳定同位素,用于表征马达加斯加高地森林砍伐和土地利用变化后土壤碳的趋势

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摘要

The impacts of human land use in the highlands of Madagascar are often equated with land degradation and decreasing soil fertility. The practice most often focused on is deforestation through slash-and-burn cultivation (tavy), and shifting cultivatorsare often portrayed as being ignorant, poverty-stricken peasants felling trees for fields and food. However, there is uncertainty whether soil degradation is related to recent tavy or earlier forest clearance, and whether some highland areas were ever forested. In this paper we use stable isotopes (gamma 513~C) and diffuse reflectance spectroscopy (DRS) to study the impacts of deforestation and various other land use changes on ecosystem properties, soil organic carbon (SOC) dynamics and soil quality (fertility) in the highlands of Madagascar. Land cover transitions (between C_3 and C_4 systems) are defined and quantified in the study area. Historical land use had greater effect on soil organic carbon concentrations than current land use, with cultivated areas previously under C_3 and C_4 systems having 37.3 and 14.8 g SOC kg~(-1), respectively. Grasslands previously under C_3 had approximately 124% more SOC than grasslands previously under C_4, while SOC concentrations were 65.3 and 54.9 g C kg~(-1)under natural forest and in mixed fallow systems, respectively. A soil fertility index developed for the study area based on diagnostic soil spectra was compared with findings related to SOC dynamics and land use change.
机译:马达加斯加高地上人类土地利用的影响通常等同于土地退化和土壤肥力下降。人们最常侧重的做法是通过刀耕火种(关税)砍伐森林,而经常将耕种者描述为无知的,贫穷的农民砍伐树木以获取田地和粮食。但是,尚不确定土壤退化是否与最近的河道治理或较早的森林砍伐有关,以及某些高地地区是否曾经造林。在本文中,我们使用稳定同位素(γ513〜C)和漫反射光谱(DRS)来研究森林砍伐和其他各种土地利用变化对生态系统特性,土壤有机碳(SOC)动态和土壤质量(肥力)的影响。马达加斯加的高原。在研究区域中定义并量化了土地覆盖转换(在C_3和C_4系统之间)。历史土地利用对土壤有机碳浓度的影响要大于当前土地利用,以前在C_3和C_4系统下的耕地分别具有37.3和14.8 g SOC kg〜(-1)。在C_3下的草地比在C_4下的草地具有更多的SOC,而在天然森林和混合休耕系统下,SOC的浓度分别为65.3和54.9 g C kg〜(-1)。将根据诊断土壤光谱为研究区域开发的土壤肥力指数与与SOC动态和土地利用变化有关的发现进行了比较。

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