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Monitoring the field soil matrix potential using mercury tensiometer and granular matrix sensors

机译:使用汞张力计和粒状基质传感器监测现场土壤基质潜力

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The monitoring of dynamic water flow is becoming progressively more important in soil erosion studies. The main aim of this paper is to evaluate monitoring techniques for soil matrix potential and data handling and use in relation to soil hydrologicdynamics. The study was developed in erosion plots at Avelar Experimental Campus, located in a mountainous region of the State of Rio de Janeiro, Brazil. Mercury manometer tensiometers and granular matrix sensors were used for the hydrologic monitoring.The hydrologic behavior in relation to the matrix potential in the erosion plots has demonstrated that the most superficial depth showed the most negative potentials as well as a quick response in relation to the drainage. In relation to the temporal variation of the matrix potential in the upper plot of the erosion plots, one can observe that the plots with different soil tillage history presented different hydrologic behavior.
机译:在土壤侵蚀研究中监测动态水流正在变得逐渐变得更加重要。本文的主要目的是评估土壤矩阵潜力和数据处理的监测技术,以及与土壤水文动力学的关系。该研究是在Avelar实验校园的侵蚀地块中开发的,位于巴西里约热内卢州的山区。水银压缩计和粒状基质传感器用于水文监测。与侵蚀图中的基质电位相关的水文行为表明,最浅的深度显示出最负面的电位以及与引流有关的快速反应。关于侵蚀地块的上图中的基质电位的时间变化,人们可以观察到具有不同土壤耕作历史的曲线呈现不同的水文行为。

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