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首页> 外文期刊>International Journal of Environmental Protection and Policy >The Impacts and Implications of Anthropogenic Forces on the Unstable Geologic Platform in Parts of Anambra and Imo States Southeastern, Nigeria
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The Impacts and Implications of Anthropogenic Forces on the Unstable Geologic Platform in Parts of Anambra and Imo States Southeastern, Nigeria

机译:人为力量对尼日利亚东南部阿南布拉州和伊莫州部分地区不稳定的地质平台的影响和影响

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Anthropogenic activities have exacerbated the incidences of floods, soil and gully erosion and landslides in parts of southeastern states of Anambra and Imo, Nigeria. Intense urbanization, deforestation, agricultural, commercial/industrial activities has extensively-denudated and elluviated the total environment. The variations in climatic condition also have associated implications. The rainy season registers an average annual rainfall of 2000 mm. The Geology comprises an unstable platform of a regional escarpment/cuesta subtended by sandy, highly-fractured and faulted Nanka sands/Ameki Formation. The underlying unstable geology facilitates the development of gullies with depth ranging from 2 m to over 80 m. The calculated rate of soil removal from the gully prone areas is about 9.20 to 10.16 ton/ha/yr. The significant cuesta of the area with steep scarp slope and gentle dip slope forms both surface and groundwater divide that also facilitates gully and landslide developments. The underlying geologic sandy structure is quite porous and permeable with huge aquiferous horizons of high pore-water pressures and effective stress. The problems of laissez faire attitude and poor understanding of the destructive implications of the unstable regional geologic platform result in the failure of measures to prevent myriads of environmental destructions and economic wastes.
机译:人为活动加剧了东南部阿南布拉州和尼日利亚伊莫州部分地区的洪水,土壤和沟壑侵蚀以及山体滑坡的发生。激烈的城市化,森林砍伐,农业,商业/工业活动广泛剥夺了整个环境。气候条件的变化也具有相关的含义。雨季的年平均降雨量为2000毫米。地质构造包括一个不稳定的平台,该平台的陡峭的悬崖/断层由砂质,高度断裂和断层的南卡砂/ Ameki地层对接。潜在的不稳定地质条件促进了沟壑的发展,其深度范围从2 m到80 m以上。从易发生沟壑区的土壤去除率的计算值约为9.20至10.16吨/公顷/年。该地区的陡峭陡峭陡坡和缓倾斜坡度的重要地块形成了地表水和地下水的分水岭,也促进了沟壑和滑坡的发展。潜在的地质砂质结构是相当多孔且可渗透的,具有巨大的含水层,具有较高的孔隙水压力和有效应力。自由放任的态度问题以及对不稳定的区域地质平台的破坏性影响的认识不足,导致无法采取措施来防止各种环境破坏和经济浪费。

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