Kaolin minerals in the Amazon soils [Brazil]

Kaolin minerals in the Amazon soils [Brazil]

The kaolin minerals in the Amazon upland soils vary ranging from the well-crystallized triclinic/b-axis disordered kaolinite intermediate in a red yellow latosol and a red yellow podzolic soil to the disordered kaolinite/halloysite (7 Å) intermediate in a "Terra Roxa Estruturada" soil and...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Soil science and plant nutrition (Tokyo) 1980-01, Vol.26 (2), p.255-269
Hauptverfasser: Kitagawa, Yasuo, Möller, Maria Regina Freire
Format: Artikel
Sprache:eng
Schlagworte:
halloysite (7 Å)
kaolinite
tropical soil
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 269
container_issue 2
container_start_page 255
container_title Soil science and plant nutrition (Tokyo)
container_volume 26
creator Kitagawa, Yasuo
Möller, Maria Regina Freire
description The kaolin minerals in the Amazon upland soils vary ranging from the well-crystallized triclinic/b-axis disordered kaolinite intermediate in a red yellow latosol and a red yellow podzolic soil to the disordered kaolinite/halloysite (7 Å) intermediate in a "Terra Roxa Estruturada" soil and a reddish brunizem. The particle size of kaolin minerals become smaller, and their structural randomness increase, with the increase of iron content of the clay fractions in the Amazon upland soils.
doi_str_mv 10.1080/00380768.1980.10431208
format Article
fullrecord <record><control><sourceid>fao_cross</sourceid><recordid>TN_cdi_crossref_primary_10_1080_00380768_1980_10431208</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>JP19810672985</sourcerecordid><originalsourceid>FETCH-LOGICAL-c336t-9d7be641cf2ab7ca8e9f5b7e1ac741aabfffeff6dcc298cc35414c7653b1e3d83</originalsourceid><addsrcrecordid>eNqFT81KxDAYDKJgXX2FpQ9g16RJm_RYF11_FvSgJ5HwNU000jaSFGT36U2pe_b0DfPNDDMILQleESzwFcZUYF6KFanERDFKciyOUEI441n8FMcomUQTFqfoLIQvjBmjRZ6gy0dwnR3S3g7aQxfSiMdPndY97N2QBmcj93btYW-793N0YqJGX_zdBXq9vXlZ32Xbp839ut5mitJyzKqWN7pkRJkcGq5A6MoUDdcEFGcEoDHGaGPKVqm8EkrRghGmYk_aEE1bQReonHOVdyF4beS3tz34nSRYTpvlYbOcNsvD5misZ6MdjPM9_DjftXKEXee88TAoGyT9N2M5ZxhwEj58tDw8RwnBJY91C_oLcfBnYw</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Kaolin minerals in the Amazon soils [Brazil]</title><source>EZB-FREE-00999 freely available EZB journals</source><creator>Kitagawa, Yasuo ; Möller, Maria Regina Freire</creator><creatorcontrib>Kitagawa, Yasuo ; Möller, Maria Regina Freire ; National Inst. of Agricultural Sciences, Yatabe, Ibaraki (Japan) ; Rijksuniversiteit, Gent (Belgium). Faculteit van de Landbouwwetenschappen</creatorcontrib><description>The kaolin minerals in the Amazon upland soils vary ranging from the well-crystallized triclinic/b-axis disordered kaolinite intermediate in a red yellow latosol and a red yellow podzolic soil to the disordered kaolinite/halloysite (7 Å) intermediate in a "Terra Roxa Estruturada" soil and a reddish brunizem. The particle size of kaolin minerals become smaller, and their structural randomness increase, with the increase of iron content of the clay fractions in the Amazon upland soils.</description><identifier>ISSN: 0038-0768</identifier><identifier>EISSN: 1747-0765</identifier><identifier>DOI: 10.1080/00380768.1980.10431208</identifier><language>eng</language><publisher>Taylor &amp; Francis Group</publisher><subject>halloysite (7 Å) ; kaolinite ; tropical soil</subject><ispartof>Soil science and plant nutrition (Tokyo), 1980-01, Vol.26 (2), p.255-269</ispartof><rights>Copyright Taylor &amp; Francis Group, LLC 1980</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c336t-9d7be641cf2ab7ca8e9f5b7e1ac741aabfffeff6dcc298cc35414c7653b1e3d83</citedby><cites>FETCH-LOGICAL-c336t-9d7be641cf2ab7ca8e9f5b7e1ac741aabfffeff6dcc298cc35414c7653b1e3d83</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>Kitagawa, Yasuo</creatorcontrib><creatorcontrib>Möller, Maria Regina Freire</creatorcontrib><creatorcontrib>National Inst. of Agricultural Sciences, Yatabe, Ibaraki (Japan)</creatorcontrib><creatorcontrib>Rijksuniversiteit, Gent (Belgium). Faculteit van de Landbouwwetenschappen</creatorcontrib><title>Kaolin minerals in the Amazon soils [Brazil]</title><title>Soil science and plant nutrition (Tokyo)</title><description>The kaolin minerals in the Amazon upland soils vary ranging from the well-crystallized triclinic/b-axis disordered kaolinite intermediate in a red yellow latosol and a red yellow podzolic soil to the disordered kaolinite/halloysite (7 Å) intermediate in a "Terra Roxa Estruturada" soil and a reddish brunizem. The particle size of kaolin minerals become smaller, and their structural randomness increase, with the increase of iron content of the clay fractions in the Amazon upland soils.</description><subject>halloysite (7 Å)</subject><subject>kaolinite</subject><subject>tropical soil</subject><issn>0038-0768</issn><issn>1747-0765</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1980</creationdate><recordtype>article</recordtype><recordid>eNqFT81KxDAYDKJgXX2FpQ9g16RJm_RYF11_FvSgJ5HwNU000jaSFGT36U2pe_b0DfPNDDMILQleESzwFcZUYF6KFanERDFKciyOUEI441n8FMcomUQTFqfoLIQvjBmjRZ6gy0dwnR3S3g7aQxfSiMdPndY97N2QBmcj93btYW-793N0YqJGX_zdBXq9vXlZ32Xbp839ut5mitJyzKqWN7pkRJkcGq5A6MoUDdcEFGcEoDHGaGPKVqm8EkrRghGmYk_aEE1bQReonHOVdyF4beS3tz34nSRYTpvlYbOcNsvD5misZ6MdjPM9_DjftXKEXee88TAoGyT9N2M5ZxhwEj58tDw8RwnBJY91C_oLcfBnYw</recordid><startdate>19800101</startdate><enddate>19800101</enddate><creator>Kitagawa, Yasuo</creator><creator>Möller, Maria Regina Freire</creator><general>Taylor &amp; Francis Group</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>19800101</creationdate><title>Kaolin minerals in the Amazon soils [Brazil]</title><author>Kitagawa, Yasuo ; Möller, Maria Regina Freire</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c336t-9d7be641cf2ab7ca8e9f5b7e1ac741aabfffeff6dcc298cc35414c7653b1e3d83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1980</creationdate><topic>halloysite (7 Å)</topic><topic>kaolinite</topic><topic>tropical soil</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kitagawa, Yasuo</creatorcontrib><creatorcontrib>Möller, Maria Regina Freire</creatorcontrib><creatorcontrib>National Inst. of Agricultural Sciences, Yatabe, Ibaraki (Japan)</creatorcontrib><creatorcontrib>Rijksuniversiteit, Gent (Belgium). Faculteit van de Landbouwwetenschappen</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><jtitle>Soil science and plant nutrition (Tokyo)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kitagawa, Yasuo</au><au>Möller, Maria Regina Freire</au><aucorp>National Inst. of Agricultural Sciences, Yatabe, Ibaraki (Japan)</aucorp><aucorp>Rijksuniversiteit, Gent (Belgium). Faculteit van de Landbouwwetenschappen</aucorp><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Kaolin minerals in the Amazon soils [Brazil]</atitle><jtitle>Soil science and plant nutrition (Tokyo)</jtitle><date>1980-01-01</date><risdate>1980</risdate><volume>26</volume><issue>2</issue><spage>255</spage><epage>269</epage><pages>255-269</pages><issn>0038-0768</issn><eissn>1747-0765</eissn><abstract>The kaolin minerals in the Amazon upland soils vary ranging from the well-crystallized triclinic/b-axis disordered kaolinite intermediate in a red yellow latosol and a red yellow podzolic soil to the disordered kaolinite/halloysite (7 Å) intermediate in a "Terra Roxa Estruturada" soil and a reddish brunizem. The particle size of kaolin minerals become smaller, and their structural randomness increase, with the increase of iron content of the clay fractions in the Amazon upland soils.</abstract><pub>Taylor &amp; Francis Group</pub><doi>10.1080/00380768.1980.10431208</doi><tpages>15</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0038-0768
ispartof Soil science and plant nutrition (Tokyo), 1980-01, Vol.26 (2), p.255-269
issn 0038-0768
1747-0765
language eng
recordid cdi_crossref_primary_10_1080_00380768_1980_10431208
source EZB-FREE-00999 freely available EZB journals
subjects halloysite (7 Å)
kaolinite
tropical soil
title Kaolin minerals in the Amazon soils [Brazil]
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-01T16%3A28%3A44IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-fao_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Kaolin%20minerals%20in%20the%20Amazon%20soils%20%5BBrazil%5D&rft.jtitle=Soil%20science%20and%20plant%20nutrition%20(Tokyo)&rft.au=Kitagawa,%20Yasuo&rft.aucorp=National%20Inst.%20of%20Agricultural%20Sciences,%20Yatabe,%20Ibaraki%20(Japan)&rft.date=1980-01-01&rft.volume=26&rft.issue=2&rft.spage=255&rft.epage=269&rft.pages=255-269&rft.issn=0038-0768&rft.eissn=1747-0765&rft_id=info:doi/10.1080/00380768.1980.10431208&rft_dat=%3Cfao_cross%3EJP19810672985%3C/fao_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true