sao VICENTE FERRER-PE市葡萄种植系统、行间、植物间和更新区域下土壤物理属性的评价

J. Silva, Sandro Augusto Bezerra
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引用次数: 0

摘要

葡萄藤是一种适应各种气候因子能力很强的植物。在巴西,“乡村葡萄”或“普通葡萄”的名称用于所有美国葡萄品种(葡萄和葡萄),以及不同品种葡萄的杂交品种。在传统农业中,由于需要在更短的时间内生产更多的产品,通常使用旨在增加产量的投入和技术,这往往对环境产生负面影响。采用有助于增加有机质含量的管理和利用做法可以改善其物理质量,例如增加保水能力,从而成为农业系统可持续管理的重要战略。本研究的目的是评价葡萄种植行间、株间和种植面积土壤的物理属性,评价其土壤密度、颗粒密度和重量水分。这项研究是在位于 o Vicente f rrer PE的Flávio先生的财产中进行的。试验设计采用分割地块,其中主要处理为三种使用系统:行间葡萄种植、植株种植和种植更新区。二级处理为0 ~ 10cm、1020cm、20 ~ 30cm、30 ~ 40cm 4层土壤剖面。结果表明,随着深度的增加,土壤密度增大,由于颗粒密度没有统计学差异,土壤湿度在最表层较高,这可以解释为有机质含量和植被覆盖度较高。存在于植物之间的区域。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
AVALIAÇÃO DOS ATRIBUTOS FÍSICOS DO SOLO SOB SISTEMA DE CULTIVO DA UVA, ENTRE LINHAS, ENTRE PLANTAS E AREA DE RENOVAÇÃO MUNICÍPIO DE SÃO VICENTE FERRER-PE
O The vine is a plant with great capacity to adapt to various edaphoclimatic factors. The name "rustic grapes" or "common grapes" is used in Brazil for all American grape cultivars (Vitis labrusca and Vitis bourquina), and hybrids of different species of Vitis. In conventional agriculture, due to the need to produce more in less time, it is common to use inputs and techniques aimed at increasing production, often negatively affecting the environment. The adoption of management and use practices that contribute to an increase in organic matter content can improve its physical qualities, increasing, for example, the water retention capacity, thus becoming an important strategy for the sustainable management of agricultural systems. The objective of this work was to evaluate the physical attributes of the soil in grape cultivation between rows, between plants and planting area, evaluating its soil density, particle density and gravimetric moisture. The research was developed in the property of Mr. Flávio located in São Vicente Férrer PE. The experimental design used was that of split plots, where the main treatments were three systems of use: Grape Cultivation between rows, plants and planting renewal area. And the secondary treatments were four layers of the soil profile: 0-10cm, 1020cm, 20-30cm and 30-40cm. In the results we can observe a higher value of soil density when we increased the depth, since the particle densities did not differ statistically, the soil moisture was higher in the most superficial soil layers, being explained by the higher organic material content and vegetation cover. present in areas between plants.
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