INFLUENCE OF TREES DENSITIES IN WATER INFILTRATION IMPROVEMENT IN AGROFORESTRY PARKLAND IN BURKINA FASO

K. Jonas, Kagambega O. Raymond, Y. Barthelemy
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Abstract

Soil structure is an essential factor in soil organic carbon sequestration. Infiltration capacity (IC) is a key property for semi-arid soils because rains in this area fall with high flows. Objective of this study was to measure soil stability in Prosopis africana agroforestry parkland with contrasted trees density. Specifically, it was to compare water infiltration rate in plots. Study was carried in Saria research station in Burkina Faso, West Africa. Design used is a factorial with three repetitions. Only one treatment was applied. This is trees density which has 4 levels: Density 0 = 0 trees per hectare (Control); Density 1 = 434 trees ha-1; Density 2 = 217 trees ha-1 and Density 3 = 109 trees ha-1. Measurement was made using a single-ring infiltrometer. Change in water depth in cylinder was measured over 2h30 at time intervals. Infiltration rate and cumulative infiltrations for each period were calculated. Results show that presence of tree density impacted significantly water infiltration rate and cumulative infiltration. Density 1 and 2 had better infiltration rate and cumulative infiltration. This result show how the presence of trees in production system could lead to water properties and/or carbon sequestration improvement in these ecosystems.
树木密度对布基纳法索农林业公园用地渗水改善的影响
土壤结构是影响土壤有机碳固存的重要因素。入渗能力(IC)是半干旱土壤的一个重要特性,因为该地区降雨大,流量大。本研究的目的是通过对比树木密度来衡量非洲藜农林业公园用地的土壤稳定性。具体来说,就是比较不同地块的水分入渗速率。研究在西非布基纳法索的Saria研究站进行。使用的设计是三次重复的阶乘。只应用了一种治疗方法。这是树木密度,有4个等级:密度0 =每公顷0棵树(对照);密度1 = 434棵ha-1;密度2 = 217棵ha-1,密度3 = 109棵ha-1。采用单环渗透计进行测量。每隔一段时间测量缸内水深的变化。计算各时段的入渗率和累计入渗量。结果表明,树木密度的存在对水分入渗速率和累积入渗有显著影响。密度1和密度2的入渗速率和累积入渗速率较好。这一结果表明,在生产系统中树木的存在如何导致这些生态系统的水性质和/或碳固存改善。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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