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Post-Fire Resource Redistribution in Desert Grasslands: A Possible Negative Feedback on Land Degradation

机译:沙漠草原火灾后的资源再分配:对土地退化的可能负面反馈

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Desert grasslands, which are very sensitive to external drivers like climate change, are areas affected by rapid land degradation processes. In many regions of the world the common form of land degradation involves the rapid encroachment of woody plants into desert grasslands. This process, thought to be irreversible and sustained by biophysical feedbacks of global desertification, results in the heterogeneous distribution of vegetation and soil resources. Most of these shrub-grass transition systems at the desert margins are prone to disturbances such as fires, which affect the interactions between ecological, hydrological, and land surface processes. Here we investigate the effect of prescribed fires on the landscape heterogeneity associated with shrub encroachment. Replicated field manipulation experiments were conducted at a shrub-grass transition zone in the northern Chihuahuan desert (New Mexico, USA) using a combination of erosion monitoring techniques, microtopography measurements, infiltration experiments, and isotopic studies. The results indicate that soil erosion is more intense in burned shrub patches compared to burned grass patches and bare interspaces. This enhancement of erosion processes, mainly aeolian, is attributed to the soil-water repellency induced by the burning shrubs, which alters the physical and chemical properties of the soil surface. Further, we show that by enhancing soil erodibility fires allow erosion processes to redistribute resources accumulated by the shrub clumps, thereby leading to a more homogeneous distribution of soil resources. Thus fires counteract or diminish the heterogeneity-forming dynamics of land degradation associated with shrub encroachment by enhancing local-scale soil erodibility.
机译:沙漠草原对诸如气候变化等外部驱动因素非常敏感,是受土地快速退化过程影响的地区。在世界许多地区,土地退化的常见形式涉及将木本植物迅速侵占沙漠草原。全球荒漠化的生物物理反馈认为这一过程是不可逆转和持续的,导致植被和土壤资源的分布不均。这些在沙漠边缘的灌木-草丛过渡系统大多数都容易受到诸如火灾之类的干扰,这些干扰会影响生态,水文和地表过程之间的相互作用。在这里,我们研究了规定的火灾对与灌木侵蚀相关的景观异质性的影响。使用侵蚀监测技术,微形貌测量,渗透实验和同位素研究相结合,在奇瓦瓦沙漠北部(美国新墨西哥州)的灌木丛过渡带进行了野外重复操作实验。结果表明,与烧过的草丛和裸露的空隙相比,烧过的灌木丛的土壤侵蚀更为严重。侵蚀过程(主要是风尘)的这种增强归因于燃烧灌木引起的土壤疏水性,从而改变了土壤表面的物理和化学性质。此外,我们表明,通过增强土壤的可侵蚀性,火灾使侵蚀过程能够重新分配灌木丛所积累的资源,从而导致土壤资源的分布更加均匀。因此,大火通过增强局部土壤的可侵蚀性来抵消或减少与灌木侵蚀相关的土地退化的异质性形成动力。

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