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Quantifying the effects of aggregation, particle size and components on the colour of Mediterranean soils
Author(s) -
SÁnchezMarañón M.,
Soriano M.,
Melgosa M.,
Delgado G.,
Delgado R.
Publication year - 2004
Publication title -
european journal of soil science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.244
H-Index - 111
eISSN - 1365-2389
pISSN - 1351-0754
DOI - 10.1111/j.1365-2389.2004.00624.x
Subject(s) - silt , particle size , soil water , mineralogy , organic matter , chemistry , particle (ecology) , scanning electron microscope , soil organic matter , particle size distribution , analytical chemistry (journal) , soil science , environmental chemistry , materials science , geology , organic chemistry , paleontology , oceanography , composite material
Summary Aggregation, particle size, and chemical composition affect the colour of the soil. We have attempted to quantify and understand these effects in 12 Mediterranean soils. We measured the CIELAB colour variables h ab , L *, and C * ab in aggregated and dispersed soil samples, and also in coarse sand, fine sand, silt, and clay samples before and after sequential removal of organic matter, carbonates, and Fe oxides. Grassmann's colour‐mixing equations adjusted by regression analysis described the colour of the dispersed soil from its particle‐size fractions with an error of 1% for h ab , 4% for L *, and 9% for C * ab . This suggests that the contribution of each fraction to the colour of the dispersed soil can be accurately calculated by its colorimetric data weighted by its content and a regression coefficient, which was greatest for clay. We inferred the influence of a component within each fraction by measuring the colour changes after its removal. Iron oxides reduced h ab of the silicated substrate by 19%, reduced L * by 12%, and increased C * ab by 64% in all particle‐size fractions. Carbonates and organic matter had little influence: the former because they impart little colour to the silicates and the latter because there was little of it. The CIELAB colour‐difference between dispersed and aggregated soil (mean Δ E * ab = 15.3) was due mainly to Δ L * (−14.7). Aggregation contributed to diminishing L * of dispersed soil by 34%. Scanning electron microscopy showed that Fe oxides and organic coatings cover the surface of aggregates thereby influencing soil colour.