Propiedades morfológicas de los suelos asociadas a los ecosistemas de Páramo, Nariño, Sur de Colombia

IF 0.3 Q4 AGRONOMY
Felipe Zúñiga Ugalde, Jenny Lucia Huertas Delgado, G. Obando, José Dörner Fernández, J. Bravo, H. Orjuela
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引用次数: 0

Abstract

Franklin Delano Roosevelt (1882-1945) stated: “A nation that destroys its soils destroys itself.” How can we get the soil closer to society so that this sentence does not become reality? One alternative is to develop didactic tools that allow socializing the information that soil profiles can provide. Soil morphological properties associated with paramo ecosystems and their link with ecosystem services (SE) were studied in Narino, Southern Colombia through a pedotransference function (FPTs) with an instructive approach, oriented to the environmental regulation of the study area. Forty-two soil horizons were described morphologically in a range of 9 ecosystems (paramos to crops). In general, the deepest soils are found in paramos and native forest systems. These soils are also dark, evidence of accumulation of soil organic carbon. Soil bulk density varied between 0.13 and 1.35 Mg m-3, and soil organic carbon ranged between 0.60 and 23.77%. This property explains soil bulk density (P < 0.0001; r2 = 0.83) and is described by an inverse first order equation. Soil organic carbon is a useful indicator to estimate quantitative aspects of the soil pore system and to infer the ecosystem services of water, air and nutrient regulation of the paramos. Finally, “Land information cards” are proposed as tools to will inform and raise awareness of the society regarding the importance of the soil as natural capital and prevent the sentence of F.D. Roosevelt from becoming an uncomfortable reality.
哥伦比亚南部paramo, narino与生态系统相关的土壤形态特性
富兰克林·德拉诺·罗斯福(Franklin Delano Roosevelt, 1882-1945)说过:“破坏土壤的国家也就是破坏自己的国家。”我们怎样才能让土壤更贴近社会,让这句话不成为现实?另一种选择是开发教学工具,使土壤剖面可以提供的信息社会化。以研究区环境调控为导向,采用土壤迁移函数(FPTs)对哥伦比亚南部Narino地区土壤形态特征及其与生态系统服务(SE)的关系进行了研究。在9个生态系统中对42个土壤层进行了形态学描述。一般来说,最深的土壤是在paramos和原生森林系统中发现的。这些土壤也是深色的,这是土壤有机碳积累的证据。土壤容重为0.13 ~ 1.35 Mg m-3,土壤有机碳含量为0.60 ~ 23.77%。这一特性解释了土壤容重(P < 0.0001;R2 = 0.83),并由反一阶方程描述。土壤有机碳是估算土壤孔隙系统定量方面和推断流域水、空气和养分调节等生态系统服务功能的有用指标。最后,“土地信息卡”被提议作为一种工具,将告知和提高社会对土壤作为自然资本的重要性的认识,并防止罗斯福的判决成为一个令人不安的现实。
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来源期刊
Terra Latinoamericana
Terra Latinoamericana Environmental Science-Ecology
CiteScore
1.10
自引率
0.00%
发文量
49
审稿时长
16 weeks
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