Gafur Gözükara, Bayram Çağdaş Demirel, S. Altunbaş
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引用次数: 1

摘要

土壤颜色是反映土壤形态、物理、化学和矿物学性质的重要数据来源。因此,在田间条件下,土壤科学家在确定土壤层边界时,从土壤颜色差异中获益良多。本研究的目的是确定A层和C层土壤对某些物理化学性质与数字颜色参数(L, A和b)之间关系的影响。在冲积地上、下带17个土壤剖面的A层和C层采集了91个土壤样品。对土壤样品进行了数字颜色参数(L、a和b)、质地、pH、电导率、石灰、有机质、可交换K、Na、Ca+Mg、阳离子交换容量(CEC)等分析。A层的L值与pH(0.77**)、石灰(0.82**)、A值与砂(0.54**)、Ca+Mg(-0.65**)、CEC(-0.65**)、b值与砂(0.52**)、Ca+Mg(-0.55**)、CEC(-0.56**)呈极显著相关。在C层,L值与粉砂(0.57**)、pH(0.65**)、石灰(0.81**)、K(-0.50**)、A值与粘土(-0.58**)、砂(0.48**)、b值与粘土(-0.55**)、石灰(0.68**)呈极显著相关。根据结果进行多元线性回归分析;利用L和a值可以确定pH值(r2 = 0.68),利用a层的a和b值可以确定石灰含量(r2 = 0.73),利用C层的L、a和b值可以确定石灰含量。结果表明,数字颜色参数可以更可靠地测定pH值和石灰含量,但这一性能受A和C水平的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Sayısal renk parametreleri ile toprak özellikleri arasındaki ilişkiye toprak horizonlarının etkisi
Soil color is an important data source about the morphological, physical, chemical and mineralogical properties of the soil. Therefore, soil scientists benefit significantly from soil color differences in determining the boundaries of soil horizons in field conditions. The aim of this research was to determine the effect of soils taken from A and C horizons on the relationship between some physical-chemical properties and digital color parameters (L, a and b). Ninety-one soil samples were taken from the A and C horizons of 17 soil profiles in the upper and lower zones of the alluvial land. Digital color parameters (L, a and b), texture, pH, electrical conductivity, lime, organic matter, exchangeable K, Na, Ca+Mg, cation exchange capacity (CEC) analyzes were performed in soil samples. A significant correlation was found between L value and pH (0.77**) and lime (0.82**), between a value and sand (0.54**), Ca+Mg (-0.65**) and CEC (-0.65**), and between b value and sand (0.52**), Ca+Mg (-0.55**) and CEC (-0.56**) in the A horizons. A significant correlation was found between L value and silt (0.57**), pH (0.65**), lime (0.81**) and K (-0.50**), between a value and clay (-0.58**), sand (0.48**), and between b and clay (-0.55**), lime (0.68**) in the C horizons. According to the results of multiple linear regression analysis; pH (R 2 = 0.68) value can be determined with L and a values, and lime (R 2 = 0.73) content can be determined using a and b values in A horizons, and lime content can be determined using L, a and b values in C horizons. It is concluded that digital color parameters can be used more reliably determining pH and lime content and this performance is affected by A and C horizons.
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