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@article{489640,
author = {Koubová, Magdaléna and Zeman, Josef and Müller, Pavel and Koubová, Magdaléna and Müller, Pavel},
article_location = {Praha},
article_number = {3},
keywords = {soil; lake bottom sediment; sandstone; clay minerals; smectite; illite; kaolinite; chlorite; carbonate cement},
language = {eng},
issn = {1214-1119},
journal = {Bulletin of Geosciences},
title = {Mineralogy, petrography and geochemistry of sediments used in pollutant sorption experiments},
url = {http://nts2.cgu.cz/servlet/page?_pageid=245,247,273&_dad=portal30&_schema=PORTAL30&453_TOC_140721.p_subid=71882&453_TOC_140721.p_sub_siteid=33&453_TOC_140721.p_edit=0},
volume = {78},
year = {2003}
}
TY - JOUR
ID - 489640
AU - Koubová, Magdaléna - Zeman, Josef - Müller, Pavel - Koubová, Magdaléna - Müller, Pavel
PY - 2003
TI - Mineralogy, petrography and geochemistry of sediments used in pollutant sorption experiments
JF - Bulletin of Geosciences
VL - 78
IS - 3
SP - 163-168
EP - 163-168
PB - Czech geological survey
SN - 12141119
KW - soil
KW - lake bottom sediment
KW - sandstone
KW - clay minerals
KW - smectite
KW - illite
KW - kaolinite
KW - chlorite
KW - carbonate cement
UR - http://nts2.cgu.cz/servlet/page?_pageid=245,247,273&_dad=portal30&_schema=PORTAL30&453_TOC_140721.p_subid=71882&453_TOC_140721.p_sub_siteid=33&453_TOC_140721.p_edit=0
N2 - Sediments from the bottom of the Horní Bečva Reservoir(HBS2,HBS6,HBV4)contain identical mineral phases andvaryinclaycontents(HBS2 1wt%,HBV4 18.5wt%).Withtheincreasingclayamount,thecontentsofFe-oxyhydroxidesandorganicmatteralsoincrease.Claymineralsinlakebottomsedimentsarerepresentedmainlybykaolinite(K),chlorite(C)andmixed-layerillite/smectite(I/S)withexpandabilityofca.40%S[(K>C)=I/S].NeogeneargillaceousandsiltysandstonefromStaréMěsto(SMA)comprisesthehighestamountofclayfraction(31wt%).Phyllosilicates,especiallysmectiteandkaolinite(S=K),surroundtherock-formingminerals.H(Hevlín)and Žd(Ždánice)PaleogeneandNeogenesiltysandstonescontaincarbonatecement(dolomite>calcite).ThedominantclaymineralinbothsandstonesisI/Swithexpandabilityofca.95%S.TheHsamplecontainsalsoaconsiderableamountofchloriteanddiscreteillite(S>C>Id). Žd samplecompriseslesskaolinitepluschloriteanddiscreteillite[S>(K>C)>Id].ThesoilhorizonfromLelekovice(Le4)istypicalinthepresenceofcarbonates,weatheredamphibolesandepidoteminerals(derivedfromametabasitesource),inhighercontentsofclayfraction(15wt%),organicmatterandFe-oxyhydroxides.ThemainclaymineralinsampleLe4ismixed-layerillite/smectitewithexpandabilityaround65%Sandkaolinite(I/S>K).ThesoilhorizonfromČervenohorskésedloSaddle(SČS5)istypicalintheabsenceoffeldspars,inthehighcontentofmuscoviteandbiotite(derivedfrommicaschists)andinthehighestamountoforganicmatterandFe-oxyhydroxides. Clay minerals of this sample include mostly discrete illite; chlorite and kaolinite are less abundant (Id > C > K).
ER -
KOUBOVÁ, Magdaléna, Josef ZEMAN a Pavel MÜLLER. Mineralogy, petrography and geochemistry of sediments used in pollutant sorption experiments. \textit{Bulletin of Geosciences}. Praha: Czech geological survey, 2003, roč.~78, č.~3, s.~163-168. ISSN~1214-1119.
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