土地利用对巴西亚马孙南部两个流域土壤物理水文属性的影响

IF 2.9 Q2 SOIL SCIENCE
Francielli Aloisio Moratelli, Marco Aurélio Barbosa Alves, Daniela Roberta Borella, Aline Kraeski, Frederico Terra de Almeida, Cornélio Alberto Zolin, Aaron Kinyu Hoshide, Adilson Pacheco de Souza
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引用次数: 0

摘要

土地利用的变化会导致土壤物理质量的退化,对环境和农业生产产生负面影响。研究了巴西南部亚马逊河流域雷纳托河和Caiabi河流域不同土地利用方式对土壤物理水文属性的影响。评估了三种土地利用条件:原生林、作物和各流域源、中、口的牧场。在0.4 m以下的3个土层中,对土壤的粒径、颗粒密度、容重、总孔隙度、大孔隙度、微孔隙度、田间容量含水量、永久萎蔫点含水量和有效水量进行了评价。收集的数据进行Kruskal-Wallis非参数检验和Pearson相关检验。采用主成分法进行多变量分析。在雷纳托流域,与原生林相比,放牧和作物的常规管理导致土壤物理退化,表层土壤密度增加,宏观孔隙度和总孔隙度降低。在Caiabi流域,将原始森林地区转变为牧场和作物改变了水质,通过降低土壤水分传导性影响了土壤中的水分动态。土壤属性因流域而异,在源头和河口之间存在质地差异,表明土壤属性的变化是由同一流域不同区域的管理和土壤颗粒组成共同造成的。采用作物和牧场保护措施可以改善亚马逊南部与农业区接壤地区的土壤物理属性。
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 Land Use on Soil Physical-Hydric Attributes in Two Watersheds in the Southern Amazon, Brazil
Changes in land use can cause degradation of soil physical quality with negative effects on the environment and agricultural production. The effects of different land uses on soil physical-hydric attributes were studied in the Renato River and Caiabi River watersheds in the southern Brazilian Amazon. Three conditions of land use were evaluated: native forest, crops, and pasture in the headwater, middle, and mouth of each watershed. Particle size, particle density, bulk density, total porosity, macroporosity, microporosity, water contents at field capacity and permanent wilting point, and available water capacity in soil were evaluated in three soil layers down to 0.4 m. Data collected were subjected to the Kruskal–Wallis nonparametric test and Pearson’s correlations. Multivariate analyses were also performed using the principal component method. In the Renato watershed, in comparison with native forest, conventional management of pasture and crops caused soil physical degradation, increasing soil density in the surface layer and reducing macroporosity and total porosity. In the Caiabi watershed, converting native forest areas into pasture and crops altered water quality, influencing the water dynamics in the soil, by reducing soil water conductivity. Soil attributes varied by watershed, with texture variations between the headwater and mouth, indicating that changes in soil properties result from both management and the granulometric composition of the soil in different regions of the same watershed. Adoption of crop and pasture conservation practices can improve soil physical attributes in regions bordering agricultural areas in the southern Amazon.
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来源期刊
Soil Systems
Soil Systems Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
5.30
自引率
5.70%
发文量
80
审稿时长
11 weeks
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