RELATIONSHIPS BETWEEN THE PETROLOGICAL NATURE AND THE CLAY MINERAL COMPOSITION OF VOLCANIC ASH SOILS DISTRIBUTED IN THE SUBURBS OF FUKUOKA-CITY, KYUSHU

スポンサーリンク

概要

• 論文の詳細を見る

• A contrasting occurrence of clay minerals was found within a soil profile which was derived from volcanic materials in the suburbs of Fukuoka-city, Northern Kyushu. The soil profile is located on an isolated terrace, and the morphological characteristics of the soil correspond exactly to Andosols, so-called Kuroboku soils or Humic Allophane soils. The clay fraction of upper horizons of the soil consists largely of alumina-rich gel-like materials, gibbsite, and layer silicates such as chlorite and chlorite-vermiculite intergrades, while that of lower horizons is composed of allophane and gibbsite or halloysite. There was no positive indication of allophane in the upper horizons. Corresponding with the clay mineralogical composition, quartz is abundant in the fine sand fraction of the upper horizons, while the mineral is very scarce or none in the lower horizons, suggesting a close relation between the petrological nature of parent volcanic materials and the mineralogical composition of weathering products. The dominant clay mineral in the volcanic soil might be dependent on the petrological nature of parent materials, and allophane is mostly formed from andesitic materials, and alumina-rich gel-like materials and layer silicates have come from quartz andesitic materials. Allophane would transform to gibbsite or halloysite according to weathering conditions, and aluminarich gel-like materials change to gibbsite under a well-drained condition. The soil materials have been so greatly weathered that some horizons contain gibbsite of even more than 40 per cent or halloysite over 70 per cent. The morphology and mineralogy are quite similar to so-called "non-volcanic Kuroboku soils."

• 社団法人日本土壌肥料学会の論文

著者

• MIZOTA Chitoshi

  Faculty of Agriculture, Iwate University

• Mizota Chitoshi

  Faculty Of Agriculture Iwate University

• AOMINE SHIGENORI

  Faculty of Agriculture, Kyushu University

• Aomine Shigenori

  Faculty Of Agriculture Kyushu University

• Mizota Chitoshi

  Faculty Of Agricultuer Iwate University

関連論文

• An Evaluation of Source Sulfur in Soft Tissues of Marine and Freshwater Benthic Animals from Japan Using Stable Isotope Analysis
• An Isotopic Characterization of Sulfur Uptake by Benthic Animals from Tsuyazaki Inlet, Northern Kyushu, Japan
• Salt Accumulation in Topsoils of lrrigated Maize Fields in Comparison with Irrigated Rice Fields in Kilimanjaro Region, Semiarid Tanzania
• EOLIAN ADDITIONS TO SOILS AND SEDIMENTS OF JAPAN
• Sulfur Isotope Composition of Soft Tissues of Deep-sea Mussels, Bathymodiolus spp., in Japanese Waters
• Stable isotopic characterization of carbon, nitrogen and sulfur uptake of Acharax japonica from central Japan
• MINERALOGY OF THE TROPOSPHERIC DUSTS IN RAINWATER COLLECTED IN FUKUOKA, NORTHERN KYUSHU
• IMOGOLITE OF CHILEAN VOLCANIC ASH SOILS
• RELATIONSHIPS BETWEEN THE INORGANIC COLLOID AND THE PARENT MATERIAL OF SOME VOLCANIC ASH SOILS IN MIYAGI AND IWATE PREFECTURES, JAPAN
• EOLIAN ORIGIN OF QUARTZ AND MICA IN SOILS DEVELOPED ON BASALTS IN NORTH-WESTERN KYUSHU AND SAN-IN, JAPAN
• RELATIONSHIPS BETWEEN THE PETROLOGICAL NATURE AND THE CLAY MINERAL COMPOSITION OF VOLCANIC ASH SOILS DISTRIBUTED IN THE SUBURBS OF FUKUOKA-CITY, KYUSHU
• EOLIAN ORIGIN OF THE MICACEOUS MINERALS IN AN ANDO SOIL FROM KITAKAMI, JAPAN
• CLAY MINERALOGY OF THE A HORIZONS OF SEVEN ANDO SOILS, CENTRAL KYUSHU
• CLAY MINERALOGY OF SOME VOLCANIC ASH SOILS IN WHICH CRISTOBALITE PREDOMINATES
• RELATIONSHIPS BETWEEN THE PRIMARY MINERAL AND THE CLAY MINERAL COMPOSITIONS OF SOME RECENT ANDOSOLS
• CLAY MINERALOGY OF A DYSTRANDEPT AND A HAPLAQUOD FROM NORTHLAND, NEW ZEALAND
• CLAY MINERALOGY OF SPODIC HORIZONS FROM CRYORTHODS IN JAPAN
• PHOSPHATE FIXATION BY ANDO SOILS DIFFERENT IN THEIR CLAY MINERAL COMPOSITION
• Origin of boulder-size euhedral quartz in the Seto Porcelain Clay Formation, central Japan
• Nitrogen isotope composition of inorganic soil nitrogen and associated vegetation under a sea bird colony on the Hatana islands, Rotuma Group, Fiji
• Process of Formation of Potentially Acid Sulfate Soils from Central Kyushu, Japan: Sulfur Isotopic Approach
• HEAT OF IMMERSION OF SOIL ALLOPHANIC CLAYS WITH ORGANIC LIQUIDS
• CLAY MINERALS FROM DIALLAGE IN A WARM AND HUMID CLIMATE
• VERMICULITE IN SOME JAPANESE SOILS
• EFFECTS OF DRYING AND HEATING ON THE SURFACE AREA OF ALLOPHANE AND IMOGOLITE
• CLAY MINERALOGY OF THE SAPROLITE OF SOME VOLCANIC ROCKS IN JAPAN
• INFLUENCE OF DISPERSION TREATMENTS ON THE PROPERTIES OF SOIL COLLOIDS
• WEATHERING OF MONTMORILLONITE IN SOILS
• WEATHERING OF MONTMORILLONITE IN TUFFACEOUS SHALES UNDER SEVERE LEACHING
• IMOGOLITE IN SOME ANDO SOILS
• Sulfur isotopic variations in soft tissues of Calyptogena soyoae from Sagami Bay, central Japan
• CLAY MINERALS OF SEDIMENTS IN THE YATSUSHIRO BAY
• CLAY MINERALS OF SOILS FROM OLIVINE BASALT IN KYUSHU
• Low sulfur isotopic signatures (δ^S) of macrozoobenthos from a brackish lagoon: contribution of microbially reduced sulfides
• DOES "ALLOPHANE B" EXIST IN JAPANESE VOLCANIC ASH SOILS?
• RETENTION OF MERCURY BY SOIL COLLOIDS : III. Adsorption of Mercury in Dilute Phenylmercuric Acetate Solutions
• FLOCCULATION OF ALLOPHANIC CLAYS BY ELECTROLYTES
• HEAT OF IMMERSION OF SOIL ALLOPHANIC CLAYS
• GRADE OF WEATHERING AND FERTILITY OF VOLCANIC ASH SOILS OF ASO VOLCANO
• IMOGOLITE OF IMOGO-LAYERS IN KYUSHU
• OCCURRENCE OF GIBBSITE IN WEATHERING OF VOLCANIC MATERIALS AT KUROISHIBARU, KUMAMOTO
• RETENTION OF MERCURY BY SOILS : I. Mercury Residues of Paddy and Orchard Soils
• EFFECTS OF ALLOPHANIC CIAYS ON THE ENZYMATIC ACTIVITY OF BETA-AMYLASE
• NITROGEN FERTILITY AND HUMIC MATTER OF CHILEAN ANDOSOLS
• RETENTION OF MERCURY BY SOILS : II. Adsorption of Phenylmercuric Acetate by Soil Colloids
• MINERALOGY OF GEL-LIKE SUBSTANCE IN THE PUMICE BED IN KANUMA AND KITAKAMI DISTRICTS
• EFFECTS OF ALLOPHANE ON THE ENZYMATIC ACTIVITY OF A PROTEASE
• MECHANISM OF INHIBITORY EFFECT OF ALLOPHANE AND MONTMORILLONITE ON SOME ENZYMES
• EFFECTS OF EXCHANGEABLE CATIONS ON THE HIGH TEMPERATURE EXOTHERMIC PEAK OF ALLOPHANE
• HYDROXY-AL COMPLEXES OF MONTMORILLONITE AND VERMICULITE AND IDENTIFICATION OF INTERGRADES OF MONTMORILLONITE-CHLORITE AND VERMICULITE-CHLORITE IN SOILS
• EFFECTS OF THE SOIL ON THE ACTIVITY OF PENTACHLOROPHENOL
• MECHANISMS OF PENTACHLOROPHENOL ADSORPTION BY SOILS
• CLAY MINERALOGY OF SEVEN DYSTRANDEPTS DEVELOPED FROM BASALTS IN NORTHLAND, THE FRENCH MASSIF CENTRAL AND WESTERN OREGON
• Process of Formation of Potentially Acid Sulfate Soils from Central Kyushu, Japan : Sulfur Isotopic Approach
• INFLUENCE OF pH ON THE FORMATION OF THE HYDROXYAl-MONTMORILLONITE COMPLEX
• ADSORPTION OF PENTACHLOROPHENOL BY SOILS
• THE pH OF CHILEAN VOLCANIC ASH SOILS "TRUMAOS"
• SO-CALLED 14 Å CLAY MINERALS IN SOME ANDO SOILS
• SOIL FABRICS OF THE PLOWED LAYER OF FLOODED RICE FIELDS

もっと見る 閉じる

スポンサーリンク