Studies on classification, dating and genetic environments of paleosols in cold climatic regions, north Japan
Project/Area Number |
62480049
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Research Category |
Grant-in-Aid for General Scientific Research (B)
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Allocation Type | Single-year Grants |
Research Field |
土壌・肥料
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Research Institution | Obihiro University of Agriculture and Veterinary Medicine |
Principal Investigator |
KONDO Yuko Professor, Obihiro University, 畜産学部, 教授 (30003081)
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Co-Investigator(Kenkyū-buntansha) |
KOSAKI Takashi Instructor, Obihiro University, 畜産学部, 助手 (00144345)
TSUCHIYA Fujio Assoc. Professor, Obihiro University, 畜産学部, 助教授 (30003130)
KONDO Renzo Assoc. Professor, Obihiro University, 畜産学部, 助教授 (30003106)
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Project Period (FY) |
1987 – 1988
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Project Status |
Completed (Fiscal Year 1988)
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Budget Amount *help |
¥3,300,000 (Direct Cost: ¥3,300,000)
Fiscal Year 1988: ¥500,000 (Direct Cost: ¥500,000)
Fiscal Year 1987: ¥2,800,000 (Direct Cost: ¥2,800,000)
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Keywords | Cold climatic region / Periglacial paleosols / Permafrost / テフロクロノロジー / 古土壌 / テフロクロノジー / 寒冷気候の古土壌 / 古土壌の分類 / 古土壌の堆積年代 / 古土壌の生成環境 / 土壌生成分類 |
Research Abstract |
The buried periglacial paleosols, involutions and earth hummocks, are often observed in Hokkaido and northeastern honshu, north Japan. The tephrochronological studies of the Late Pleistocene periglacial phenomena are carried out and the paleopedology in the investigation area is also discussed. In the Tokachi Plain of the eastern Hokkaido, fossil periglacial paleosols in the Late Pleistocene such as involutions were found at many places in the buried volcanic ash soils. Ages of these pale-osols are considered to be well correlative to the cold climatic stages of the Late Pleistocene revealed by plant opal analyses and by floral assemblages. A sporadic permafrost is distributed in the vicinity of Tokachi-mitsumata, northernmost Tokachi District. This relict permafrost (ca.1.3-4.0m deep and ca.26,500m^2 in area) is know only on the NNW steep slope of above 830-886m in altitude. Since the ^<14>C dating made on wood sample collected in the lowermost level of the frozen layer indicate 4,540 105 yrs. B.P.. Annual soil temperature at 0.5m depth is -4.3゜C. The morphology and nature of the involutions in the buried volcanic ash soils, sporadic permafrost and earth hummocks; and their geographical distribution are briefly given in this report.
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Report
(3 results)
Research Products
(22 results)