演替农林复合系统中与土壤肥力相关的变量——苏德斯特山脉,RS,巴西

Daniel Hanke, Shirley Grazieli da Silva Nascimento, Déborah Pinheiro Dick, Renan Costa Beber Vieira, Leonardo Paz Deble
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摘要

演替农林复合系统具有提高土壤肥力和恢复退化生态系统的能力。本研究的目的是调查农林业系统在不同生态演替阶段对巴西南部地区土壤化学和物理肥力属性动态的影响。土壤样品在五种不同条件下采集:i)控制(T) =初始系统(不含农林业);ii) SAF1 =发展1年的农林业;SAF3 = 3年发展的农林业;SAF7 =发展7年的农林业;参考系统(30年自然再生森林)。随后,决定/化学属性的计算进行了参数(可交换的Ca + 2毫克+ 2 K +、Na + P + 3, H +,基地,有效的和潜在的阳离子交换能力,阳离子交换饱和与基地和基地+ 3),物理属性(土壤容重、粒子密度、总孔隙度、水分),和土壤理化性质(酸碱H 2 O,在盐的解决方案,和SMP方法),并根据各采样层的土壤质量计算化学元素储量。结果表明,随着体系发育时间的延长,pH值、总孔隙度和养分储量均有所增加,而酸度成分则有所减少。土壤肥力的变化与土壤有机质含量的增加有直接关系。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Variables related to soil fertility in successional agroforestry systems – Serras do Sudeste, RS, Brazil
Abstract Successional agroforestry systems have the capacity to increase soil fertility and restore degraded ecosystems. The objective of this study was to investigate the influence of agroforestry systems, at different stages of ecological succession, on the dynamics of chemical and physical soil fertility attributes in the Brazil South region. Soil samples were collected under five different conditions: i) Control (T) = initial system (without agroforestry); ii) SAF1 = agroforestry with 1 year of development; iii) SAF3 = agroforestry with 3 years of development; iv) SAF7 = agroforestry with 7 years of development; and v) reference system (naturally regenerating forest with 30 years). Subsequently, determinations/calculations were carried out for chemical attributes/parameters (exchangeable Ca + 2 , Mg + 2 , K + , Na + , P, Al + 3 , H + , sum of bases, effective and potential cation exchange capacity, cation exchange saturation with bases and Al + 3 ), physical attributes (soil bulk density, particle density, total porosity, and moisture), and soil physicochemical properties (pH H 2 O, pH in saline solutions, and SMP method), as well as chemical element stocks were calculated based on soil mass in each sampled layer. Results indicated an increase in pH, total porosity, and nutrient stocks with the systems' development time, accompanied by a decrease in acidity components. The change in soil fertility is directly related to the increase in soil organic matter content.
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