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Indicative Recognition Criteria of Degradation by Compaction of the Greenhouses Soils with Coarse Texture

机译:用粗糙纹理的温室土壤压实指示性识别标准

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Soil with coarse texture (clay<12%) are known under the name of Psamosol [1,2], Arenosol [3] or Psament [4] and belong to loamy texture class or coarser. In the French classification system Arenosol correlate with taxa within the "Classe de sol minereaux" and "Classe de sol peu evolues". These soils have low water-holding capacities, high water permeability, excessive aeration, low content of all essential nutrients, low buffer capacity and are still much less fertile than most soils in the regions they are located in. the sandy or loamy sand soil are susceptible to physical degradation by wind erosion and compaction processes [5]. Soil vulnerability to compaction increase if the fine sand/coarse sand ratio is lower than 10 [6]. Coarse textured soils are considered warm because heat up soil easily due to low water holding capacity. Plants grown on these soils arrive maturity earlier about 2-3 weeks compared to those grown on soils with finer texture in the same climate zone. Since the incipient degradation of the sandy or loamy sand soil is harder noticed by farmers, in this paper we proposed a set of indirect indicators for assessing the status of soil degradation, especially by compaction. Proposed set of indicators refers to plants uniformity, the local presence of areas with stagnant growth plants, the shape areas, the accumulation of slightly soluble salts on the soil surface, uniformity moist band after drip irrigation. Main conclusions: (i) Greenhouses soils with coarse texture (clay content lower than 12%) have high susceptibility to degradation by physical and chemical processes. (ii) Dimensions of moistened soil band, after irrigation administration, is an good indirect indicator for assessing the state of compaction of soils. (iii) We consider that developing a chart to determine the state of soil compaction on indirect indicators is useful for farmers because are easy to follow and to measure.
机译:粗糙纹理(粘土<12%)的土壤是在Psamosol [1,2],氨基溶胶[3]或psament的名称下已知的,并且属于植物纹理类或粗糙。在法国分类系统中,氨纶与“Classe de Sol Minereaux”中的分类群相关联,“Classe de Sol Peu Evolues”。这些土壤的水持续能力低,水渗透性高,过度曝气,低含量,所有必需营养素的含量低,缓冲量低,仍然比它们所在地区的大多数土壤更低的肥沃。砂质或壤土易受风蚀和压实过程的物理降级的影响[5]。如果细砂/粗砂比低于10 [6],则压实的土壤脆弱性增加。粗糙织地不细土壤被认为是温暖的,因为由于低水量的容量而容易加热土壤。与在相同气候区的越细纹的土壤上成长,这些土壤种植的植物在其上午2-3周内到达成熟。由于农民注意到砂质或壤土土壤的初始退化,因此,在本文中,我们提出了一系列间接指标,用于评估土壤退化状态,特别是通过压实。提出的指标指的是植物均匀性,局部存在具有停滞不前的生长植物,形状区域,在土壤表面上略微可溶的盐的积累,滴灌后的均匀性潮湿带。主要结论:(i)温室土壤具有粗糙质地(粘土含量低于12%)对物理和化学方法的降解敏感性高。 (ii)灌水管理后润湿的土壤带的尺寸是评估土壤压实状态的良好间接指标。 (iii)我们认为,制定图表以确定间接指标对农民有用的土壤压实状态,因为很容易遵循和测量。

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