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首页> 外文期刊>Soil & Tillage Research >Gypsum effects on the spatial distribution of coffee roots and the pores system in oxidic Brazilian Latosol
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Gypsum effects on the spatial distribution of coffee roots and the pores system in oxidic Brazilian Latosol

机译:石膏对氧化巴西Latosol中咖啡根的空间分布和毛孔系统的影响

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摘要

The aim of this study was to jointly evaluate the root system and soil pore distribution in depth and their relation to the development of the coffee cop. Three trenches were dug at random, longitudinal to the plant row, in a very clayey oxidic Latosol (Oxisol), subject to the following dose of gypsum: GO: absence of additional gypsum; G7: 7 Mg ha(-1); and G28: 28 Mg ha(-1) of additional gypsum, both applied on the surface in the plant row. For the root system evaluation we used the crop profile method associated with 2D image analyzes, and subsequent elaboration of root variables maps. Soil pores system was quantified in 3D images, originated by X-ray CT scan, in undisturbed soil cores (0.06 m diameter and 0.14 m high) sampled at 0.20-0.34; 0.80-0.94; and 1.50-1.64m depth. Roots and pores were classified by diameter. The statistical inferences were performed in R language. The increasing doses of gypsum favored the development of fine roots efficient in water absorption, and the highest gypsum dose promoted the better spatial distribution of the root system and was more homogeneous in the vertical direction of the soil profile, with highlighting to G28. The highest pore number and volume occurs in the 0.20-0.34 m structural layer, particularly pores with a diameter less than 2 mm. This management system that employs high gypsum doses contributed beneficially to a new structural organization in all depth studied, and most meaningful at 0.20-0.34 m depth, especially with the increase of pores and expertise of roots (smallest diameter: 1 mm) contributing to better exploitation of the soil conditions by the coffee plant. Image analyses are an tool with high predictive power to evaluated soil pores and roots system without destruction of the soil structure. (C) 2014 Elsevier B.V. All rights reserved.
机译:这项研究的目的是共同评估根系和土壤孔隙深度分布及其与咖啡品种发展的关系。在非常黏稠的氧化型Latosol(Oxisol)中,在与植物行垂直的位置随机挖出三个沟渠,施用以下剂量的石膏:GO:不存在额外的石膏; G7:7 Mg ha(-1);和G28:28 Mg ha(-1)的额外石膏,均施加在植物行的表面上。对于根系评估,我们使用了与2D图像分析相关的作物剖面方法,以及随后对根系变量图的详细说明。在X射线CT扫描产生的3D图像中,以0.20-0.34采样的未扰动土壤核(直径0.06 m和高0.14 m)对土壤孔隙系统进行了定量; 0.80-0.94;和1.50-1.64m深度。根和孔按直径分类。统计推断使用R语言进行。不断增加的石膏剂量有利于细根的吸水发展,而最高的石膏剂量则促进了根系更好的空间分布,并且在土壤剖面的垂直方向上更均匀,突出显示为G28。最高的孔数和最大的体积出现在0.20-0.34 m的结构层中,特别是直径小于2 mm的孔。该管理系统采用高剂量的石膏,有利于研究所有深度的新型结构组织,并且在0.20-0.34 m的深度最有意义,尤其是随着孔的增加和根系的专长(最小直径:1 mm),其效果更好。咖啡厂对土壤条件的利用。图像分析是一种具有高预测能力的工具,可以评估土壤孔隙和根系,而不会破坏土壤结构。 (C)2014 Elsevier B.V.保留所有权利。

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