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Soil Erosion Management Practices in the Prefecture of Kilkis, Northern Greece

机译:基尔基斯县土壤侵蚀管理实践,希腊北部

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Declining yield, as a result of erosion in soils located in the Prefecture of Kilkis, Northern Greece has been observed. An area of about 3.000 hectares has been studied and the majority of the examined soils were mainly formed from the weathering of limestone or acidic material. These soils cover mainly hilly areas, have been classified as Entisols, Inceptisols or Alfisols, and are usually cultivated by wheat, maize, cotton, tobacco and sugar beets. They have been developed on tertiary or quaternary deposits and the upper terraces or alluvial fun are very susceptible to erosion. The appearance of high degree of erosion is present in the slopes greater than 6 % and is illustrated in the erosion map. Pronounced differences on soil depth, texture, water holding capacity, and nutrients have been recorded. Available phosphorus was very low in the subsurface layers, whilst potassium ranges in the ploughing layers and magnesium was in normal levels. Nutrient loss is quite severe and nitrogen leaching seems to play a dominant role in the decline of the crop yield, hence on farmers income. Attention should be paid hi the water shortage during the dry season, which affect land cover and erosion risk is increased during the rainy season, hi particular, it can be argued that in this semi-arid region the following measures and practices may be adopted such as: the policy of subsidies which encourage farmers for rotation or set aside of marginal areas, incentives for reforestation, minimum ploughing and/or ploughing along contour-lines, rational irrigation by means of the extension of drip irrigation systems may be applied, avoidance the burning of plant residues after harvesting and hi general adoption of a sustainable land use planning may be introduced.
机译:已经观察到,由于位于基尔基斯县(Kilkis)的土壤侵蚀而导致的产量下降。已经研究了约3.000公顷的面积,主要的审查的土壤主要由石灰石或酸性材料的耐候形成。这些土壤主要覆盖主要是丘陵地区,已被归类为奥斯索尔,升中或阿尔芬斯,通常由小麦,玉米,棉花,烟草和甜菜培养。他们已经在第三节或第四纪沉积物上开发,上露台或冲积乐趣非常容易受到侵蚀。高度侵蚀的外观存在于大于6%的斜坡中,并在侵蚀地图中示出。已经记录了土壤深度,质地,水持能力和营养素的明显差异。可用的磷在地下层中非常低,而犁吹层和镁的钾范围是正常水平。营养损失是非常严重的,氮浸出似乎在作物产量的下降中发挥着主导作用,因此对农民收入的衰退。在旱季期间,应注意净水缺水,影响陆地覆盖和侵蚀风险在雨季,嗨,特别是,可以认为,在这个半干旱地区,可能采取以下措施和实践as:鼓励农民旋转或搁置边缘地区的补贴政策,反射搅动的激励,沿着轮廓线的耕犁和/或犁,通过延伸滴灌系统的合理灌溉,避免收获后的植物残留物燃烧,可以介绍一般采用可持续土地使用规划。

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