Quantification of soil features using digital image processing (DIP) techniques

被引:47
作者
Aydemir, S [1 ]
Keskin, S
Drees, LR
机构
[1] Harran Univ, Fac Agr, Dept Soil Sci, TR-63043 Sanliurfa, Turkey
[2] Soil & Water Natl Informat Ctr, Gen Directory Rural Serv, Ankara, Turkey
[3] Texas A&M Univ, Dept Soil & Crop Sci, College Stn, TX 77843 USA
关键词
digital image processing; quantification; soil features; micromorphology; image classification; image processing;
D O I
10.1016/S0016-7061(03)00218-0
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
A new thin section method is introduced which provides reliable, automated classification of mineral, non-mineral constituents (e.g. organic matter), non-crystalline, or poorly crystalline components (e.g. Fe-Mn oxides) and voids. A color image flatbed scanner scanned 10 soil thin section slides that contain the same features. Equal portions, (about 6.3 cm(2)) of each slide were imported into the Erdas Image Processing software (version 8.4) as 24 bit 3-band images. Images were classified with an unsupervised nearest neighbor classification method with several different processing steps. Five different classes were separated and quantified, for each sample. Classified features were checked with 500 reference, points under the petrographic microscope. Separation and identification was almost 100% for calcite, about 97% for void in all samples, but values decreased for sesquioxides, plasma, and quartz (96%, 96%, and 80%, respectively). Quantitative results of digital image processing based on pixel number of each class (aerial percentage) were compared with traditional point-counting method.. Digital image processing results showed slightly lower values for voids, quartz and sesquioxides, but higher values for plasma and almost equal quantity for calcite in all three samples when compared with the values of the point-counting method. This technique represents a significant improvement in quantitative soil micromorphology. Requirement of simple and inexpensive hardware and quick and routine identification and. quantification of features (calcite, void, sesquioxides, and plasma) with much less error than other methods are two advantages of the proposed method to the earlier studies. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:1 / 8
页数:8
相关论文
共 35 条
  • [1] Colour description and quantification in mosaic images of soil thin sections
    Adderley, WP
    Simpson, IA
    Davidson, DA
    [J]. GEODERMA, 2002, 108 (3-4) : 181 - 195
  • [2] [Anonymous], SOIL MICROMORPHOLOGY
  • [3] AYDEMIR S, 2001, THESIS TEXAS A M U
  • [4] MEASUREMENT OF PORE-SIZE DISTRIBUTION IN A LAMELLAR BT HORIZON USING EPIFLUORESCENCE MICROSCOPY AND IMAGE-ANALYSIS
    BOUABID, R
    NATER, EA
    BARAK, P
    [J]. GEODERMA, 1992, 53 (3-4) : 309 - 328
  • [5] Brewer R., 1976, FABRIC MINERAL ANAL
  • [6] QUANTIFICATION OF SOIL CALCIUM CARBONATES BY STAINING AND IMAGE-ANALYSIS
    BUI, EN
    MERMUT, AR
    [J]. CANADIAN JOURNAL OF SOIL SCIENCE, 1989, 69 (03) : 677 - &
  • [7] TOWARDS THE QUANTIFICATION OF SOIL STRUCTURE
    BULLOCK, P
    MURPHY, CP
    [J]. JOURNAL OF MICROSCOPY-OXFORD, 1980, 120 (DEC): : 317 - 328
  • [8] Campbell J.B., 1987, INTRO REMOTE SENSING
  • [9] CHAYES F, 1949, AM MINERAL, V34, P1
  • [10] COLOR M, 1998, MUNSELL SOIL COLOR C