作为不同用途和管理地区土壤质量指标的聚合度

Renato Sinquini de Souza , Igor Sousa de Morais , Jean Sérgio Rosset , Thadeu de Melo Rodrigues , Arcângelo Loss , Marcos Gervasio Pereira
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引用次数: 0

摘要

这项研究旨在评估不同的土地利用方式(植被覆盖和种植系统截然不同)对聚集物(生物和物理聚集物)的形成途径及其化学和物理属性的影响。研究在巴西巴拉那州西部地区的瓜伊拉市进行。研究选取了五种处理方法:传统耕作系统(SPC)、实施 6 年(SP6)和 18 年(SP18)的免耕系统、种植 45 年的永久性牧场(PP)以及原生林参考区(NF)。每个区域都从 0.00-0.05 米和 0.05-0.10 米土层中采集了四个土块(未扰动样本)。根据聚集体的形成途径将其分为生物成因和物理成因,并对其化学属性、聚集体稳定性、颗粒大小、土壤有机质(SOM)的密度分馏和碳(13C)的天然丰度进行了表征。在 CTS 地区,两种聚集体形成途径的 pH 值都较低,生物聚集体的钙(Ca2+)含量最低。在 NTS18 区域,两种形成途径的 SOM 含量都有所增加,量化值与在 NF 区域观察到的值相似,与 CTS 区域相比,总有机碳 (TOC) 含量以及 SOM 的易腐和难腐部分都有所增加。在林区形成的聚合体与在其他系统中形成的聚合体之间存在显著差异,这表明不同的途径可用作土壤质量的指标。通过对生物成因和物理成因聚集体中的化学和物理参数进行评估,可以通过主成分分析将研究区域分开,重点是 NTS18,它与其他区域分开,表明长期保护管理提高了矿物有机质和总有机碳的水平。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Aggregation as soil quality indicator in areas under different uses and managements

This study aimed to evaluate the influence of different land uses, with contrasting vegetation covers and planting systems, on the formation pathways of aggregates (biogenic and physicogenic) and on their chemical and physical attributes. The study was conducted in the municipality of Guaíra in the western region of the state of Paraná, Brazil. Five treatments were selected for the study: an area with a conventional tillage system (SPC), no-till system with 6 years (SP6) and 18 years (SP18) of implementation, permanent pasture (PP) with 45 years of planting, and reference area with native forest (NF). In each area, four soil blocks (undisturbed samples) were collected from the 0.00–0.05 and 0.05–0.10 ​m layers. Aggregates were classified according to their formation pathways as biogenic or physicogenic, and the chemical attributes, aggregate stability, particle size, density fractionation of soil organic matter (SOM), and natural abundance of carbon (13C) were characterized. In the CTS area, lower pH values were observed for both aggregate formation pathways, and biogenic aggregates had the lowest calcium (Ca2+) content. In the NTS18 area, there was an increase in SOM content for both formation pathways, and the quantified values were similar to those observed in the NF area, with increase in total organic carbon (TOC) content and in the labile and recalcitrant fractions of SOM when compared with those of CTS. Significant differences were observed between aggregates formed in the forest area and those formed in other systems, indicating that different pathways can be used as indicators of soil quality. The chemical and physical parameters evaluated in the biogenic and physicogenic aggregates allowed the separation of the study areas through principal component analysis, with an emphasis on NTS18, which was separated from the other areas, demonstrating that long-term conservation management increased the mineral organic matter and TOC levels.

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