Mineralogy, petrography and geochemistry of sediments used in
pollutant sorption experiments

J 2003

Mineralogy, petrography and geochemistry of sediments used in pollutant sorption experiments

KOUBOVÁ, Magdaléna, Josef ZEMAN and Pavel MÜLLER

Basic information

Original name

Mineralogy, petrography and geochemistry of sediments used in pollutant sorption experiments

Authors

KOUBOVÁ, Magdaléna (203 Czech Republic), Josef ZEMAN (203 Czech Republic, guarantor) and Pavel MÜLLER (203 Czech Republic)

Edition

Bulletin of Geosciences, Praha, Czech geological survey, 2003, 1214-1119

Other information

Language

English

Type of outcome

Článek v odborném periodiku

Field of Study

Geochemistry

Country of publisher

Czech Republic

Confidentiality degree

není předmětem státního či obchodního tajemství

References:

URL

RIV identification code

RIV/00216224:14310/03:00008999

Organization unit

Faculty of Science

Keywords in English

soil; lake bottom sediment; sandstone; clay minerals; smectite; illite; kaolinite; chlorite; carbonate cement

Abstract

V originále

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).

Links

MSM 143100004, plan (intention)

Name: Geologické procesy a jejich environmentální vyústění - styk variscid a alpid

Investor: Ministry of Education, Youth and Sports of the CR, Geological Processes and their Environmental Impact - Contact of the Variscides and Alpides

Citovat

KOUBOVÁ, Magdaléna, Josef ZEMAN and Pavel MÜLLER. Mineralogy, petrography and geochemistry of sediments used in pollutant sorption experiments. Bulletin of Geosciences. Praha: Czech geological survey, 2003, vol. 78, No 3, p. 163-168. ISSN 1214-1119.

@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 and Pavel MÜLLER. Mineralogy, petrography and geochemistry of sediments used in pollutant sorption experiments. \textit{Bulletin of Geosciences}. Praha: Czech geological survey, 2003, vol.~78, No~3, p.~163-168. ISSN~1214-1119.

Detailed Information on Publication Record