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首页> 外文期刊>American Journal of Environmental Protection >Effect of Slope Position on Soil Physico-Chemical Properties with Different Management Practices in Small Holder Cultivated Farms of Abuhoy Gara Catchment, Gidan District, North Wollo
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Effect of Slope Position on Soil Physico-Chemical Properties with Different Management Practices in Small Holder Cultivated Farms of Abuhoy Gara Catchment, Gidan District, North Wollo

机译:北沃洛吉丹地区小棚户耕种Abuhoy Gara集水区的坡地位置对不同管理方式下土壤理化性质的影响

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The research work was conducted on eroded soil at the Abuhoy Gara Catchment, which is located in the Gidan District of North Wello Zone in the Amhara National Regional State to determine the effect of slope position on soil physico-chemical properties. Soil samples were collected from higher-slope, middle slope, intermediate slope and lower slope positions at two depths, surface (0-15 cm) and subsurface (15-30 cm) soil layers. Results showed a significant difference among the physicochemical properties of higher, middle, intermediate and lower slope soils. Clay fraction of the lower slope (27.08%) was the highest followed by middle slope (26.67%), intermediate slope (23.34%) and higher slope (22.92%). Conversely, sand (60%) was highest at higher slope and followed by middle slope (57.08%), intermediate slope (51.67%) and lower slope (49.58%), respectively. Likewise, Ca (8.41 cmol(+)/ kg), Mg (3.19cmol(+)/ kg), K (1.43cmol(+)/ kg), CEC (17.58cmol(+)/ kg), total nitrogen (0.104%), organic carbon (1.88%) and Available phosphorous (9.52 ppm) at higher slope followed by middle slope, intermediate slope and lower slope, respectively. The deterioration in chemical properties of lower slope as compared to other slopes were presumed to be due to continuous cultivation for longer period of time and past soil erosion effect that removed the soil organic matter and other plant nutrients. This study results concluded that increasing extent of continuous and intensive cultivation with minimum conservation practices and erosion due to slope effect can further deteriorate soil properties. The control of such damaging effects would require proper soil conservation strategies such as proper land leveling, afforestation, crop rotation, fallowing, terracing and inclusion of restorative crops in cropping systems on these lands.
机译:该研究工作是在位于阿姆哈拉国家地区北部韦罗地区北吉丹地区的阿布霍伊加拉流域的侵蚀土壤上进行的,以确定斜坡位置对土壤理化性质的影响。在两个深度(表层(0-15厘米)和地下(15-30厘米))土壤深度的高坡度,中坡度,中坡度和低坡度位置收集土壤样品。结果表明,高,中,中,低坡土的理化性质之间存在显着差异。低坡度的粘土比例最高(27.08%),其次是中坡度(26.67%),中坡度(23.34%)和高坡度(22.92%)。相反,砂土(60%)在较高的坡度处最高,其次是中坡(57.08%),中坡(51.67%)和低坡(49.58%)。同样,Ca(8.41 cmol(+)/ kg),Mg(3.19cmol(+)/ kg),K(1.43cmol(+)/ kg),CEC(17.58cmol(+)/ kg),总氮(0.104 %),有机碳(1.88%)和有效磷(9.52 ppm),分别在较高的斜率,随后的中斜率,中间的斜率和较低的斜率下。据推测,与其他斜坡相比,下坡化学性质的下降是由于长时间连续耕种和过去的土壤侵蚀作用而去除了土壤有机质和其他植物养分所致。这项研究结果得出结论,以最小限度的保护做法增加了连续和集约耕作的范围,以及由于边坡效应造成的侵蚀会进一步恶化土壤特性。要控制这种破坏性影响,就需要采取适当的土壤保护策略,例如适当的土地平整,绿化,作物轮作,休耕,梯田化以及将恢复性作物纳入这些土地上的种植系统。

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