Impacts of Pollutants (Phosphorus and Nitrogen) from Agricultural Activities on the Soils and Waters of Toho Lake (Benin)

L. Tometin, W. Chouti, N. Chitou, Rodolphe Sotondji, J. Fatombi, D. Mama, L. Bawa
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Abstract

We evaluated the impacts of agricultural activities on the cultivated soils around Lake Toho as well as the waters from the streams through phosphorus, nitrogen and potassium pollution of the soils and waters from the streams heading towards Lake. In the soil, pHwater and pHKCl organic matter, moisture total phosphorus and its fractionation were determined. The various supernatants obtained are analyzed using a 1600PC UV spectrophotometer as well as the waters for the determination of ammonium, nitrite, nitrates and phosphate. In soils, the determination of ammonium, nitrite, nitrate, phosphate and potassium was carried out by DR 5000 MP-AES spectrometry method. Soils around this lake are weakly acidic with an average water pH of 6.91. The humidity increases from surface to depth (8% to 28%), while organic matter (11% on average) and organic carbon decrease from surface to depth. These soils are rich in phosphorus with an overall average concentration of 10.10 mg/g. The fractionation made it possibe to extract the following forms of phosphorus in soil in the order: P-residual > P-org&Al > P-Ca > P-Fe > P-Labile. The physicochemical analysis of the waters show that these waters are moderately loaded and present an increased risk of eutrophication with multifaceted consequences. In soils, nitrate is the dominant form of nitrogen. Cultivated soils provide an abundant source of nitrogen and phosphorus nutrients to Lake Toho via its recharge sources.
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农业活动污染物(磷、氮)对贝宁托霍湖土壤和水体的影响
本研究评估了农业活动对东湖周边耕地土壤和河流水体的影响,通过对土壤和流入湖泊的河流水体的磷、氮、钾污染来评估农业活动对土壤和河流水体的影响。测定了土壤中pHwater、pHKCl有机质、水分、全磷及其分异。用1600PC紫外分光光度计分析所得的各种上清液以及用于测定铵、亚硝酸盐、硝酸盐和磷酸盐的水。采用DR 5000 MP-AES光谱法测定土壤中铵、亚硝酸盐、硝酸盐、磷酸盐和钾的含量。湖周围土壤呈弱酸性,平均pH值为6.91。湿度从表层到深层增加(8% ~ 28%),有机质和有机碳从表层到深层平均减少(11%)。这些土壤磷含量丰富,总体平均浓度为10.10 mg/g。通过分选,土壤中磷的提取形式依次为:残磷>有机磷和铝磷>钙磷>铁磷>不稳定磷。对这些水域的理化分析表明,这些水域的含盐量适中,富营养化的风险增加,带来多方面的后果。在土壤中,硝酸盐是氮的主要形式。耕地土壤通过补给源为东湖提供了丰富的氮磷养分来源。
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