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Geomorphic, morphometric and structural analysis of North West Benin Owena River Basin, Nigeria: implications for groundwater development

机译:尼日利亚西北贝宁欧文纳河流域的地貌,形态计量学和结构分析:对地下水开发的影响

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An approach detailing geomorphic, morphological and structural characteristics of a basin provides insight into groundwater development in data scarce regions. Remote sensing and GIS aids the identification, extraction and mapping of these characteristics. In this study, the geomorphic, morphological and structural parameters were delineated for North West Benin Owena River Basin (NWBORB), Nigeria towards its groundwater development. The basin was delineated from topographic maps. Five major sub-basins (SB I-V) were generated. Basin geomorphic characteristics were obtained from fundamental topographic information. Each sub-basin was quantitatively assessed of for their geomorphic, morphometric (linear, areal, and relief) and structural aspects. Geomorphic, morphological and structural parameters relevant to groundwater were utilized for sub-basin prioritization and identification of deficit/surplus groundwater zones. NWBORB is a sixth order basin. Dominated by rain fed lower order streams, it reflects late youth to early mature stage of development of the fluvial geomorphic cycle. It has a low stream frequency (F_s) and moderate drainage density (D_d) of 1.149. Bifurcation ratio (R_b) shows that the lower stream orders are surging through highly dissected, steep mountainous terrain that creates a seasonal low groundwater prospect, with exceptions occurring in the pediplains and flood plain areas. A comparison of the predominant orientations of the second, third and fourth stream orders with the lineament directions indicates structural control within the basin. Sustainable water conservation techniques are suggested locally within the drainage basin. SB-II is the most deficit zone, while SB-V is found to be surplus zone of groundwater potential.
机译:一种详细描述流域地貌,形态和结构特征的方法,可以深入了解数据稀缺地区的地下水发育。遥感和GIS有助于识别,提取和绘制这些特征。在这项研究中,勾勒出尼日利亚西北贝宁欧文纳河流域(NWBORB)的地貌,形态和结构参数,以适应其地下水的发展。从地形图上划定了盆地。生成了五个主要子流域(SB I-V)。盆地地貌特征是从基本地形信息获得的。对每个子流域的地貌,形态(线性,面积和起伏)和结构方面进行了定量评估。与地下水有关的地貌,形态学和结构参数被用于次流域划分优先次序和确定缺水/过剩地下水区。 NWBORB是一个六阶盆地。雨水以低级河水为主,它反映了青年晚期至河流地貌周期发展的早期成熟阶段。它的水流频率(F_s)低,排水密度(D_d)为1.149。分岔比(R_b)表明,下游河段正在通过高度解剖的陡峭山地汹涌澎that,这形成了季节性的地下水低位前景,而在平原和泛滥平原地区则例外。第二,第三和第四流阶的主要方向与线性方向的比较表明了盆地内的结构控制。建议在流域内局部采用可持续节水技术。 SB-II是最缺水的区域,而SB-V被认为是地下水潜力的过剩区域。

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