Thresholds of gully erosion in the coastal plains sands of southeastern Nigeria

C. Udosen
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Abstract

The concept of geomorphic threshold as applied in gully erosion studies assumes that water erosion occurs when the combined power of the rainfall energy and overland flow exceeds the resistance of surface materials to detachment and entrainment. This line of reasoning presupposes that certain environmental factors that affect runoff generation and erodibility status of soil can be used in estimating thresholds for gully initiation and sustenance. The entire 413. Km2 Ikpa River basin was covered with grids 1km2 and random number table was used to select 15% of the target population in the basin. The pair-wise correlation technique was employed to establish the threshold values of vegetation cover, organic matter content, relief, slope gradient, litter cover and bulk density for gully incision and development in the fifth order drainage basin underlain by Coastal Plains Sands in eastern Nigeria. The results of the analyses indicate that the threshold value of vegetation cover was 72.5%, while the thresholds value of depth of litter cover was 3.2cm. Other threshold values for gully initiation in the catchment area were 1 degree for slope gradient; 2.70% for organic matter; and 10metres a.s.l for relief. These threshold values were exceeded in almost all the sampled gully sites. The results of the research have implications for cropping in the study area. The convectional rain-storms that is associated with the beginning of the planting season in April/May cannot be controlled by man. Its effects can be reduced to desirable level by increasing the surface contact cover. Mulching, intercropping and the planting of cover crops can ensure adequate vegetation cover of >72.5% on valley –side slopes. Also, crop residue, dry stalks and stovers should be used to encourage the build-up of organic matter above the critical level of 2.70% during the planting season. KEYWORDS: Gully erosion, threshold, Ikpa river, coastal plains, morphometry, intrinsic factors
尼日利亚东南部沿海平原沙地沟壑侵蚀的阈值
在沟壑侵蚀研究中应用的地貌阈值概念假定,当降雨能量和地表水流的总和超过地表物质对剥离和夹带的阻力时,就会发生水侵蚀。这条推理路线的前提是,某些影响径流产生和土壤可蚀性状况的环境因素可用于估计沟壑形成和维持的阈值。整个413。Ikpa河流域以1km2的网格覆盖,采用随机数字表法选择流域内15%的目标人口。利用两两相关技术建立了尼日利亚东部沿海平原沙下覆的5级流域沟槽切割发育的植被覆盖度、有机质含量、起伏度、坡度、凋落物盖度和容重阈值。分析结果表明,植被覆盖度阈值为72.5%,凋落物覆盖深度阈值为3.2cm。集水区沟壑形成的其他阈值为坡度1度;有机质占2.70%;还有10米的a.s.l.。这些阈值在几乎所有采样的沟壑区都被超过。研究结果对研究区种植具有指导意义。与四、五月播种季节开始有关的对流性暴雨是人类无法控制的。通过增加表面接触覆盖度,可以将其影响降低到理想的水平。覆盖、间作和种植覆盖作物可保证谷边坡的植被覆盖度>72.5%。此外,应利用作物残茬、干秸秆和秸秆,以促进有机质在种植季节积累到2.70%以上的临界水平。关键词:沟蚀,阈值,伊克帕河,沿海平原,形态计量学,内在因素
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