维多利亚湖流域斯米峪湿地金属分布及其对农业的影响

L. Henry, F. Mamboya
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引用次数: 3

摘要

四密峪湿地地区70%以上的居民是农牧民。土地物理退化和土壤-植物系统内养分流动性差已对农业生产产生显著影响。研究了四密峪湿地的生态循环及其对农业的影响。研究了土壤的阳离子交换容量(CEC)对可溶性阳离子和选定的微量金属的影响。为研究四密峪湿地金属元素的纵向和空间分布,在四密峪河口、四密峪大桥和巴里堤大桥3个站点采集了水、沉积物和土壤样品。在离河流不同距离的土壤中取样,以研究金属的流动模式,从而解释循环的方向。在旱季和湿季都进行了采样,以研究金属的季节变化。利用地理定位系统对土壤和水/沉积物采样点进行定位。采用原子吸收分光光度计(AAS)对金属铬(Cr)、铅(Pb)、锌(Zn)、铜(Cu)、镉(Cd)和锰(Mn)进行了分析。在大多数样品中检测到高水平的锰和锌,这些样品在水和沉积物之间的分布行为不同,这可能反映了金属在水中溶解度的差异,或者金属可能形成复合物,导致金属的溶解度降低,从而延缓了它们对低阳离子交换能力植物的生物利用度。在粘土中,由于形成了坚硬的平底锅,导致植物对养分的可利用性降低,从而促进了养分的迁移。该研究提出了一些农民可以提高土壤阳离子交换能力从而提高农业生产力的方法。DOI: http://dx.doi.org/10.3126/jowe.v6i0.5967生态学报,2012 (6):31-43
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distribution of Metals along Simiyu Wetland of Lake Victoria Basin and its Impact on Agriculture
More than 70% of communities living along Simiyu wetland area are agriculturalists and pastoralists. Physical land degradation and poor nutrient mobility within the soil-plant system have shown a notable impact on agricultural production. Cycling of selected and their impact on agriculture were investigated along Simiyu wetland. Cation Exchange Capacity (CEC) of the soil was studied with respect to soluble cations and selected trace metals. To study the longitudinal and spatial distribution of the selected metals along Simiyu wetland, samples (water, sediments and soil) were taken in three stations along the river namely Bariadi Bridge, Simiyu Bridge and the Simiyu River mouth. Sampling of soil was done at different distances from the river so as to study the flow pattern of the metals and hence to explain the direction of cycling. Sampling was done both inn wet and dry seasons to study the seasonal variation of the metals. Geographical Position System was used to locate the sampling points for soil and water/sediment. Metals Chromium (Cr), Lead (Pb), Zinc (Zn), Coper (Cu), Cadmium (Cd) and Manganese (Mn) analyses were analyzed by atomic absorption spectrophotometer (AAS). High levels of Manganese and Zinc were detected in most samples with different distribution behavior between water and sediments that may reflect difference in solubility of metals in water or possible complex formation of the metals resulting to potentially less solubility of metals, hence retarding their bioavailability to plants low cation exchange capacity. Retarded nutrient mobility in clay soils was observed facilitated by the formation of hard pans resulting to less availability of the nutrients to plants. The study suggests some ways in which farmers can improve soil cation exchange capacity and hence improve agricultural productivity. DOI: http://dx.doi.org/10.3126/jowe.v6i0.5967 J Wet Eco 2012 (6): 31-43
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