首页> 外文期刊>Progress in Physical Geography >Inaccessible Andean sites reveal human-induced weathering in grazed soils
【24h】

Inaccessible Andean sites reveal human-induced weathering in grazed soils

机译:无法访问的安第斯山脉遗址揭示了人为导致的放牧风化

获取原文
获取原文并翻译 | 示例
           

摘要

Human activity affects properties and development of ecosystems across the globe, to such a degree that it is now challenging to get baseline values for undisturbed ecosystems. This is especially true for soil development, which is potentially affected by land-use history and holds a legacy of past human interventions. Therefore, it is still largely unknown for most ecozones how soil would have developed 'naturally'. Here, we show undisturbed soil development, i.e. the processes of weathering and accumulation of soil organic matter (SOM), by comparing pristine with grazed sites in the high Andes (4500 m) of southern Peru. We located study plots on a large ledge (0.2 km~2) that is only accessible with mountaineering equipment. Plots with pristine vegetation were compared to rangeland plots that were presumably under relatively constant grazing management for at least four millennia. Vegetation change, induced by grazing management, led to lower vegetation cover of the soil, thereby increasing soil surface temperatures and soil acidification. Both factors increased weathering in rangeland soils. Formation of pedogenic oxides with high surface area explained preservation of SOM, with positive feedback to acidification. Higher contents of pyrophosphate extractable Fe and Al oxides indicated the importance of organo-mineral associations for SOM stabilization on rangeland sites, which are likely responsible for a higher degree of humification. This higher degree of humification induced melanization (darker colour) of the rangeland soils which, together with sparse vegetation cover, also feeds back to soil temperature. With this work, we present a conceptual framework of positive feedback links between human-induced vegetation change, soil development and accumulation of SOM, which is only possible due to the unique baseline values of a pristine ecosystem. Using 'inaccessibility' as a tool to quantify human impact in future interdisciplinary studies may push research forward on evaluating anthropogenic impact on Earth's ecosystems.
机译:人类活动影响着全球生态系统的性质和发展,以至于要获得不受干扰的生态系统的基准值现在是一个挑战。对于土壤开发而言尤其如此,因为土壤开发可能会受到土地使用历史的影响,并且具有过去人类干预的传统。因此,对于大多数生态区来说,土壤如何“自然”发育仍然是一个未知数。在这里,我们通过比较秘鲁南部安第斯山脉(4500 m)高处的原始和放牧地点,显示了未受干扰的土壤发育,即风化和土壤有机质积累的过程。我们将研究区放置在只有登山设备才能进入的大壁架(0.2 km〜2)上。将原始植被的土地与牧场地进行比较,据推测,牧场地处于至少四个千年以来相对稳定的放牧管理之下。放牧管理引起的植被变化导致土壤植被覆盖率降低,从而增加了土壤表面温度和土壤酸化程度。这两个因素都增加了牧场土壤的风化作用。具有高表面积的成岩氧化物的形成解释了SOM的保存,对酸化具有正反馈。焦磷酸盐可提取的Fe和Al氧化物的含量较高,表明有机-矿物缔合对于牧场地表的SOM稳定很重要,这可能是造成较高的腐殖化程度的原因。较高程度的腐化导致牧场土壤的黑色化(深色),再加上稀疏的植被覆盖,也使土壤温度升高。通过这项工作,我们提出了人为造成的植被变化,土壤发育和SOM积累之间的正反馈联系的概念框架,这仅由于原始生态系统的独特基线值才可能实现。使用“不可接近性”作为量化人类在未来跨学科研究中的影响的工具可能会推动有关评估人为对地球生态系统影响的研究。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号