Gypsum effects on the spatial distribution of coffee roots and the pores system in oxidic Brazilian Latosol

被引:22
作者
Carducci, C. E. [1 ]
Oliveira, G. C. [2 ]
Curi, N. [2 ]
Heck, R. J. [3 ]
Rossoni, D. F. [4 ]
de Carvalho, T. S. [2 ,5 ]
Costa, A. L. [2 ]
机构
[1] Fed Univ Santa Catarina Curitibanos Campi UFSC, BR-89520000 Curitibanos, SC, Brazil
[2] Dept Fed Univ Lavras DCS UF1A, BR-37200000 Lavras, MG, Brazil
[3] Univ Guelph, Sch Environm Sci, Guelph, ON N1G 2W1, Canada
[4] State Univ Maringa UEM, Dept Stat, BR-87020900 Maringa, Parana, Brazil
[5] Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England
关键词
Conservation management; X-ray CT scan; Roots distribution; Soil pores system; Image analysis; SOIL; CALCIUM; MAGNESIUM; PASTURE; REGION; YIELD;
D O I
10.1016/j.still.2014.09.015
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
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.
引用
收藏
页码:171 / 180
页数:10
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