Clay minerals in the stream floodplain soils in undisturbed landscapes of the Southern Taiga (with the soil of the state central forest nature and biosphere reserve as an example)
An X-ray diffraction technique was used to study the composition of clay material from floodplain soddy- and mucky gley soils formed in the valleys of small streams in the reserve. The content of nonexpandable minerals was higher and the labile mineral content was lower in the fine fractions of the...
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| Published in: | Moscow University soil science bulletin Vol. 68; no. 4; pp. 154 - 163 |
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| Abstract | An X-ray diffraction technique was used to study the composition of clay material from floodplain soddy- and mucky gley soils formed in the valleys of small streams in the reserve. The content of nonexpandable minerals was higher and the labile mineral content was lower in the fine fractions of the floodplain soils than in similar fractions of upland soils found in adjacent positions. Two types of disordered mixed-layered not found in upland soils-namely, illite-chlorites and chlorite-vermiculites with a variable proportion of individual layeres-were detected in the clay material. Both types of mixed-layer minerals are supposed to originate from stony fragments containing phyllosilicates of supergenic or post-magmatic origin. |
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| AbstractList | An X-ray diffraction technique was used to study the composition of clay material from floodplain soddy- and mucky gley soils formed in the valleys of small streams in the reserve. The content of nonexpandable minerals was higher and the labile mineral content was lower in the fine fractions of the floodplain soils than in similar fractions of upland soils found in adjacent positions. Two types of disordered mixed-layered not found in upland soils-namely, illite-chlorites and chlorite-vermiculites with a variable proportion of individual layeres-were detected in the clay material. Both types of mixed-layer minerals are supposed to originate from stony fragments containing phyllosilicates of supergenic or post-magmatic origin. An X-ray diffraction technique was used to study the composition of clay material from floodplain soddy- and mucky gley soils formed in the valleys of small streams in the reserve. The content of nonexpandable minerals was higher and the labile mineral content was lower in the fine fractions of the floodplain soils than in similar fractions of upland soils found in adjacent positions. Two types of disordered mixed-layered not found in upland soils-namely, illite-chlorites and chlorite-vermiculites with a variable proportion of individual layeres-were detected in the clay material. Both types of mixed-layer minerals are supposed to originate from stony fragments containing phyllosilicates of supergenic or post-magmatic origin.[PUBLICATION ABSTRACT] |
| Author | Sokolova, T. A Tolpeshta, I. I Maksimova, Yu. G Rusakova, E. S |
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| Cites_doi | 10.1134/S1064229310070082 10.1180/0009855033840106 10.3103/S0147687407030064 10.1346/CCMN.1968.0160206 10.2136/sssaj1988.03615995005200050055x 10.1134/S1064229310080065 10.3103/S0147687410030014 10.1346/CCMN.1968.0160305 |
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| References | KarathanasisADCompositional and solubility relationships between aluminum-hydroxyinterlayered soilsmectites and vermiculitesSoil Sci. Soc. Am. J.1988521500150810.2136/sssaj1988.03615995005200050055x AlekseevaSADronovaTYaSokolovaTAChemical and mineralogical characteristics of podzolic and boggy-podzolic soils developed from two-layered deposits in the Central Forest State Biospheric ReserveMoscow Univ. Soil Sci. Bull.200762314010.3103/S0147687407030064 SokolovaTADronovaTYaTolpeshtaIIGlinistye mineraly v pochvakh2005 SawhneyBLAluminum interlayers in layer silicates. Effect of oh/Al ratio of Al solution, time of reaction, and type of structureClays Clay Minerals19681615716310.1346/CCMN.1968.0160206 CarsteaDDFormation of hydroxyl-Al and -Fe interlayers in montmorillonite and vermiculite: influence of particle size and temperatureClays Clay Miner.19681623123810.1346/CCMN.1968.0160305 BarnhiselRIBerschPMChlorites and Hydroxy-Interlayered Vermiculite and Smectite. Minerals in Soil Environmets1989MadisonSoil Sci. Soc. Am. Dobrovol’skiiGVPochvy rechnykh poim tsentra Russkoi ravniny1968(Soils Bottomlands of Russian Plane’s Center) DixonJBSchulzeDGSoil Mineralogy with Environmental Application2002 MooreDMReynoldsRCJr.X-Ray Diffraction and the Identification and Analysis of Clay Minerals1997New YorkOxford SokolovaTADronovaTYaTolpeshtaIIIvanovaSEVzaimodeistvie lesnykh suglinistykh podzolistykh pochv s model’nymi kislymi osadkami i kislotnoosnovnaya bufernost’ podzolistykh pochv2001(Interaction between Forest Loam Podzol Soils and Simulated Acid Precipitations and Acid-Base Buffer Capacity of Podzolic Soils) DobrovinskayaGRUrusevskayaISOrganic matter of Southern Taiga catenas soilsVestn. Mosk. Univ., Ser. 17. Pochvoved.1999 Clays Clay Minerals1968161 Vorob’evaLAKhimicheskii analiz pochv1998(Chemical Analysis for Soils) DritsVAStructural and chemical heterogeneity of layer silicates and clay mineralsClay Minerals20033840343210.1180/0009855033840106 KovdaVAOsnovy ucheniya o pochvakh1973(Foundations of Soil Science) Clays Clay Minerals1986345 KiryushinAVSokolovaTADronovaTYaMineralogical composition of fine fractions in podzolic and gleyic peat-podzolic soils on two-layered deposits in the Central Forest State ReserveEur. Soil Sci.200235111202 KovrigoVPKaurichevISBurlakovaLMPochvovedenie s osnovami geologii2000(Soil Science and Foundations of Geology) SokolovaTATrofimovSYaTolpeshtaIIClay Minerals in the Central Forest State Reserve soils according to the problem of their genesis and classificationVestn. Mosk. Univ., Ser. 17. Pochvoved.1990 TolpeshtaIISokolovaTAMobile aluminum compounds in soils of the Southern Taiga (soils of the Central Forest Reserve as an example)Eur. Soil Sci.201043889310.1134/S1064229310080065 TolpeshtaIISokolovaTABonifacioEFalconeGPedogenic chlorites in podzolic soils with different intensities of hydromorphism: origin, properties, and conditions of their formationEur. Soil Sci.201043777710.1134/S1064229310070082 Clays Clay Minerals1969166 MeunierAClays2005Berlin, HeidelbergSpringer Verlag Regulyatornaya rol’ pochv v funktsionirovanii taezhnykh ekosistem (Soils Regulatory Role in Taiga Ecosystems Functioning), Moscow, 2002. AidinyanRKhIzvlechenie ila iz pochv: Kratkaya instruktsiya1960(Clay Extraction from Soils. Short Guide) IshkovaIVRusakovaESTolpeshtaIISokolovaTASoils of slopes and bottomland positions of the small stream valley in the Central Forest Reserve: chemical properties and clay mineralogyMoscow Univ. Soil Sci. Bull.20106539910.3103/S0147687410030014 DM Moore (4158_CR23) 1997 VA Drits (4158_CR19) 2003; 38 LA Vorob’eva (4158_CR3) 1998 A Meunier (4158_CR22) 2005 RKh Aidinyan (4158_CR1) 1960 TA Sokolova (4158_CR12) 2001 (4158_CR25) 1968; 16 (4158_CR18) 2002 GR Dobrovinskaya (4158_CR4) 1999 IV Ishkova (4158_CR6) 2010; 65 4158_CR10 II Tolpeshta (4158_CR14) 2010; 43 RI Barnhisel (4158_CR16) 1989 AV Kiryushin (4158_CR7) 2002; 35 VP Kovrigo (4158_CR9) 2000 DD Carstea (4158_CR17) 1968; 16 TA Sokolova (4158_CR13) 1990 AD Karathanasis (4158_CR20) 1988; 52 (4158_CR24) 1986; 34 (4158_CR21) 1969; 16 SA Alekseeva (4158_CR2) 2007; 62 TA Sokolova (4158_CR11) 2005 II Tolpeshta (4158_CR15) 2010; 43 BL Sawhney (4158_CR26) 1968; 16 VA Kovda (4158_CR8) 1973 GV Dobrovol’skii (4158_CR5) 1968 |
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| SubjectTerms | alluvial soils Clay clay minerals Earth and Environmental Science Earth Sciences Forests Genesis and Geography of Soils Historical Geology Landscape ecology landscapes mineral content Minerals Paleontology Soils streams taiga Taiga & tundra upland soils valleys X-ray diffraction |
| Title | Clay minerals in the stream floodplain soils in undisturbed landscapes of the Southern Taiga (with the soil of the state central forest nature and biosphere reserve as an example) |
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