埃塞俄比亚吉尔吉尔吉布流域热带农业土壤磷损失模拟

Y. Adela, C. Behn, M. Janssen, B. Lennartz
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引用次数: 2

摘要

磷是植物的重要营养物质,但由于农田磷流失过多,导致水体富营养化。位于埃塞俄比亚西南部的Gilgel gibe水库暴露于这一现象,其水质被归类为中营养型,P浓度为0.86 mg/l。本研究的目的是确定农业用地经营性磷流失机制,量化磷出口量,并利用最佳管理实践(BMPs)概念评估磷流失因素。因此,本研究采用试验数据和年磷损失估算(apple)模型来研究其潜在过程。调查了水库周围作为耕地和牧场的连片林地。在三个斜坡位置采集表土样品并进行分析。土壤主要为灰壤,小部分为垂壤,母质为玄武岩和流纹岩。利用耕地土壤数据和水文记录建立了apple模型。模拟了2001 ~ 2010年的磷损失。此外,利用实验P吸收数据对模型输出的逻辑一致性进行了检验。平均每年损失12.66±0.7 kg磷,以颗粒态和总溶解态磷的形式损失。通常,56%的磷以颗粒态磷的形式因侵蚀而损失,44%的磷以土壤溶解态和肥料直接径流态磷的形式损失。泥沙和土壤溶解态磷损失之间存在显著差异(P值= 0.000),这归因于控制磷动态的土壤化学和物理性质。显然,从农田到吉尔吉贝河和水库的主要磷转移是颗粒态磷的损失。利用bmp对导致因素的评估表明,沉积物减少5-20%导致磷从2-9%保留。同样,降低土壤磷含量可使磷损失减少2-8.5%。然而,在相同百分比范围内减少田间施肥量,相对于先前的因素,几乎不能减少磷的损失。因此,要重视精准农业的应用,避免出现这样的问题。
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Modelling Phosphorus Losses from Tropical Agricultural Soils in Gilgel Gibe Watershed, Ethiopia
Phosphorus (P) is a vital nutrient for plants, however its excess loss from agricultural lands cause eutrophication on aquatic environment. The Gilgel gibe reservoir located in the southwest part of Ethiopia is exposed to this phenomenon whereby the water quality has been classified as mesotrophic with P concentration of 0.86 mg/l. The objectives of this study were to identify the operating P loss mechanisms from agricultural lands, quantify the amount of P exported and evaluate the factors for P loss using the best management practices (BMPs) concepts. Therefore, experimental data and the annual phosphorus loss estimation (APLE) model were used to study the underlying processes. Catenas surrounding the reservoir, used as arable and pastureland, were investigated. Topsoil samples were taken and analyzed at three slope positions. The soils are mainly nitisol and a smaller portion of vertisol where the parent materials are basalt and rhyolite. The APLE model was set using soil data from the arable lands with nitisol soil and hydrologic records. The phosphorus loss was simulated from 2001 to 2010. Besides, the experimental P sorption data were used to check the logical consistency of the model output. On average 12.66 ± 0.7 kg P ha-1 yr-1 is lost in the form of particulate and total dissolved P. Generally, 56% of P is lost in the form of particulate P due to erosion, and 44% as soils dissolved and direct fertilizer runoff P. A significant variation observed between the sediment and soil dissolved P loss (p-value= 0.000) which is attributed to the soil chemical and physical properties that control the phosphorus dynamics. Obviously the dominant P transfer from agricultural lands into the Gilgel Gibe River and reservoir is particulate P loss. An evaluation of causing factors using BMPs indicated that a reduction of sediment by 5-20% resulted to retain P from 2-9%. Similarly, a reduction of soil P content reduces the P loss from 2-8.5%. However, a reduction of fertilizer quantity applied on the fields within the same percent range is hardly reducing P loss relative to the earlier factors. Therefore, attention should be given to the application of precision agriculture to avoid such problems.
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