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1. Identity statement
Reference TypeJournal Article
Sitemtc-m16c.sid.inpe.br
Holder Codeisadg {BR SPINPE} ibi 8JMKD3MGPCW/3DT298S
Identifier6qtX3pFwXQZ3P8SECKy/Ets66
Repositorysid.inpe.br/jeferson/2004/12.15.15.24   (restricted access)
Last Update2006:06.14.04.18.28 (UTC) administrator
Metadata Repositorysid.inpe.br/jeferson/2004/12.15.15.24.53
Metadata Last Update2018:06.04.04.12.58 (UTC) administrator
Secondary KeyINPE-11825-PRE/7176
ISBN/ISSN0016-7061
ISSN0016-7061
Citation KeyDematteCamAlvFioNan:2004:NeApSo
TitleVisible-NIR reflectance: a new approach on soil evaluation
Year2004
MonthJuly
Access Date2024, Apr. 27
Secondary TypePRE PI
Number of Files1
Size1324 KiB
2. Context
Author1 Dematte, Jose A. M.
2 Campos, Rogerio C.
3 Alves, Marcelo C.
4 Fiorio, Peterson R.
5 Nanni, M. R.
Group1 DPI-INPE-MCT-BR
Affiliation1 Dematte JAM (reprint author), Univ Sao Paulo, ESALQ, Dept Soil & Plant Nutr, POB 9, Piracicaba, SP BR-13418900 Brazil
2 Univ Sao Paulo, ESALQ, Dept Soil & Plant Nutr, Piracicaba, SP BR-13418900 Brazil
3 Univ Estadual Maringa, Dept Agron, Maringa, Parana Brazil
4 Natl Inst Spatial Res, INPE, Sao Jose Dos Campos, Brazil
JournalGeoderma
Volume121
Number1-2
Pages95-112
History (UTC)2004-12-15 17:24:55 :: sergio -> marciana ::
2006-03-16 19:19:40 :: marciana -> administrator ::
2006-09-27 21:01:18 :: administrator -> marciana ::
2008-05-02 16:20:27 :: marciana -> administrator ::
2018-06-04 04:12:58 :: administrator -> marciana :: 2004
3. Content and structure
Is the master or a copy?is the master
Content Stagecompleted
Transferable1
Content TypeExternal Contribution
Keywordsespectroscopia
reflectãncia espectral
análise radiométrica
radiometric analysis
toposequence
soil mapping
weathering
spectral reflectance
oxide minerals
spectroscopy
limitations
management
AbstractThe aim of this work was to develop a spectral reflectance (SR)-based methodology to evaluate soil types and soil tillage systems. Soil samples, located along nine toposequences with basalt and shale, were collected in Sao Paulo State, Brazil. SR of soil samples was measured with a laboratory spectroradiometer between 450 and 2500 nm. SR curves were evaluated at different depths to determine soil classes, as for conventional methods of soil classification. Soil survey maps were developed by descriptive interpretation of the spectral curves and statistical analysis as well. These maps were compared with detailed and semidetailed soil maps based on chemical, physical and mineralogical soil attributes (conventional method). Organic matter, total iron, silt, sand and mineralogy (quartz, magnetite, kaolinite and smectite) were the most important attributes influencing reflectance intensity and spectral features and allowed characterization and discrimination of soils. Strong absorption features centered at 1900 nm were related to OH molecules in free water of 2:1 minerals. Identification of soil classes was most precise when the entire spectral curve of different depths was analysed simultaneously, including features and intensities. Parent material variation along toposequences and weathering variability modified soil characteristics and its respective SR data. The detection of these alterations was essential to determine soil line demarcation. Soil line demarcation and number of soil classes detected by SR analyses were similar to the detailed soil map determined by conventional methods. SR laboratory measurements can be used as a methodology to assist soil surveys. Spectral data can also group soils under similar tillage systems. (C) 2003 Elsevier B.V. All rights reserved.
AreaSRE
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4. Conditions of access and use
Languageen
Target Filevisible.pdf
User Groupadministrator
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sergio
Visibilityshown
Copy HolderSID/SCD
Archiving Policydenypublisher denyfinaldraft24
Read Permissiondeny from all and allow from 150.163
5. Allied materials
Next Higher Units8JMKD3MGPCW/3EQCCU5
DisseminationWEBSCI
Host Collectionsid.inpe.br/mtc-m18@80/2008/03.17.15.17
6. Notes
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