Basic Study on the Frost Heave Pressure of Rocks: Dependence of the Maximum Frost Heave Pressure on Temperature
In this study, we attempted to measure frost heave pressure, i.e., the pressure that develops in the heat-flow direction when rocks are subject to frost heave and ice lenses grow. We used two kinds of rock samples: one was Ohya tuff, whose frost heave was already known to be high, and the other was...
Gespeichert in:
| Veröffentlicht in: | Journal of MMIJ 2011/07/25, Vol.127(8), pp.485-496 |
|---|---|
| Hauptverfasser: | , , , , , , , |
| Format: | Artikel |
| Sprache: | eng ; jpn |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 496 |
|---|---|
| container_issue | 8 |
| container_start_page | 485 |
| container_title | Journal of MMIJ |
| container_volume | 127 |
| creator | NAKAMURA, Dai GOTO, Takashi ITO, Yoji KIM, Hakusam YAMASHITA, Satoshi KAWAGUCHI, Takayuki YAMASAKI, Shintaro SUZUKI, Teruyuki |
| description | In this study, we attempted to measure frost heave pressure, i.e., the pressure that develops in the heat-flow direction when rocks are subject to frost heave and ice lenses grow. We used two kinds of rock samples: one was Ohya tuff, whose frost heave was already known to be high, and the other was Kimachi sandstone, whose frost heave was lower than that of the former. Ohya tuff and Kimachi sandstone, in which the occurrence of frost heave has previously been confirmed, were used as specimens. To conduct the experiment, we made original frost heave experiment equipment that was combined with a reaction frame and a load cell. The test results clearly showed that the maximum frost heave pressure did not depend on the kind of rock and was proportional to the temperature gradient. In addition, we clarified that the speed of the increase in pressure was proportional to the frost heave rate — the growth rate of the ice lens. |
| doi_str_mv | 10.2473/journalofmmij.127.485 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_jstag</sourceid><recordid>TN_cdi_proquest_miscellaneous_1022893420</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>1022893420</sourcerecordid><originalsourceid>FETCH-LOGICAL-j1560-d187f89c895ce0bb27ae1670d9b0192dfd913222cf03cdf01ca7a76d5399a05f3</originalsourceid><addsrcrecordid>eNpVkF1LwzAYhYMoOKc_QcilN51vkrZJLnU4NxgoflyHLB-utW1m0gr795ZNBG_OORcP5-JB6JrAjOac3dZhiJ1ugm_bqp4Ryme5KE7QhAiRZ5AXcHrYJCsJEefoIqUaoJRQiAmCe50qg1_7we5x6HC_dXgRQ-rx0ulvh5-jS2mIDgePX4L5TJfozOsmuavfnqL3xcPbfJmtnx5X87t1VpOihMwSwb2QRsjCONhsKNeOlBys3ACR1HorCaOUGg_MWA_EaK55aQsmpYbCsym6Of7uYvgaXOpVWyXjmkZ3LgxJEaBUSJZTGNHVEa1Trz-c2sWq1XGvdOwr0zj1z48a_ShxyNHSH2O2OirXsR8ZYmUn</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1022893420</pqid></control><display><type>article</type><title>Basic Study on the Frost Heave Pressure of Rocks: Dependence of the Maximum Frost Heave Pressure on Temperature</title><source>J-STAGE (Japan Science & Technology Information Aggregator, Electronic) Freely Available Titles - Japanese</source><source>EZB-FREE-00999 freely available EZB journals</source><creator>NAKAMURA, Dai ; GOTO, Takashi ; ITO, Yoji ; KIM, Hakusam ; YAMASHITA, Satoshi ; KAWAGUCHI, Takayuki ; YAMASAKI, Shintaro ; SUZUKI, Teruyuki</creator><creatorcontrib>NAKAMURA, Dai ; GOTO, Takashi ; ITO, Yoji ; KIM, Hakusam ; YAMASHITA, Satoshi ; KAWAGUCHI, Takayuki ; YAMASAKI, Shintaro ; SUZUKI, Teruyuki</creatorcontrib><description>In this study, we attempted to measure frost heave pressure, i.e., the pressure that develops in the heat-flow direction when rocks are subject to frost heave and ice lenses grow. We used two kinds of rock samples: one was Ohya tuff, whose frost heave was already known to be high, and the other was Kimachi sandstone, whose frost heave was lower than that of the former. Ohya tuff and Kimachi sandstone, in which the occurrence of frost heave has previously been confirmed, were used as specimens. To conduct the experiment, we made original frost heave experiment equipment that was combined with a reaction frame and a load cell. The test results clearly showed that the maximum frost heave pressure did not depend on the kind of rock and was proportional to the temperature gradient. In addition, we clarified that the speed of the increase in pressure was proportional to the frost heave rate — the growth rate of the ice lens.</description><identifier>ISSN: 1881-6118</identifier><identifier>EISSN: 1884-0450</identifier><identifier>DOI: 10.2473/journalofmmij.127.485</identifier><language>eng ; jpn</language><publisher>The Mining and Materials Processing Institute of Japan</publisher><subject>Frames ; Frost ; Frost Heave ; Frost Heave Pressure ; Frost Heave Rate ; Heave ; Ice Lens ; Lenses ; Rock ; Rocks ; Sandstone ; Temperature Gradient ; Tuff</subject><ispartof>Journal of MMIJ, 2011/07/25, Vol.127(8), pp.485-496</ispartof><rights>2011 The Mining and Materials Processing Institute of Japan</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,1882,27923,27924</link.rule.ids></links><search><creatorcontrib>NAKAMURA, Dai</creatorcontrib><creatorcontrib>GOTO, Takashi</creatorcontrib><creatorcontrib>ITO, Yoji</creatorcontrib><creatorcontrib>KIM, Hakusam</creatorcontrib><creatorcontrib>YAMASHITA, Satoshi</creatorcontrib><creatorcontrib>KAWAGUCHI, Takayuki</creatorcontrib><creatorcontrib>YAMASAKI, Shintaro</creatorcontrib><creatorcontrib>SUZUKI, Teruyuki</creatorcontrib><title>Basic Study on the Frost Heave Pressure of Rocks: Dependence of the Maximum Frost Heave Pressure on Temperature</title><title>Journal of MMIJ</title><addtitle>J.MMIJ</addtitle><description>In this study, we attempted to measure frost heave pressure, i.e., the pressure that develops in the heat-flow direction when rocks are subject to frost heave and ice lenses grow. We used two kinds of rock samples: one was Ohya tuff, whose frost heave was already known to be high, and the other was Kimachi sandstone, whose frost heave was lower than that of the former. Ohya tuff and Kimachi sandstone, in which the occurrence of frost heave has previously been confirmed, were used as specimens. To conduct the experiment, we made original frost heave experiment equipment that was combined with a reaction frame and a load cell. The test results clearly showed that the maximum frost heave pressure did not depend on the kind of rock and was proportional to the temperature gradient. In addition, we clarified that the speed of the increase in pressure was proportional to the frost heave rate — the growth rate of the ice lens.</description><subject>Frames</subject><subject>Frost</subject><subject>Frost Heave</subject><subject>Frost Heave Pressure</subject><subject>Frost Heave Rate</subject><subject>Heave</subject><subject>Ice Lens</subject><subject>Lenses</subject><subject>Rock</subject><subject>Rocks</subject><subject>Sandstone</subject><subject>Temperature Gradient</subject><subject>Tuff</subject><issn>1881-6118</issn><issn>1884-0450</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNpVkF1LwzAYhYMoOKc_QcilN51vkrZJLnU4NxgoflyHLB-utW1m0gr795ZNBG_OORcP5-JB6JrAjOac3dZhiJ1ugm_bqp4Ryme5KE7QhAiRZ5AXcHrYJCsJEefoIqUaoJRQiAmCe50qg1_7we5x6HC_dXgRQ-rx0ulvh5-jS2mIDgePX4L5TJfozOsmuavfnqL3xcPbfJmtnx5X87t1VpOihMwSwb2QRsjCONhsKNeOlBys3ACR1HorCaOUGg_MWA_EaK55aQsmpYbCsym6Of7uYvgaXOpVWyXjmkZ3LgxJEaBUSJZTGNHVEa1Trz-c2sWq1XGvdOwr0zj1z48a_ShxyNHSH2O2OirXsR8ZYmUn</recordid><startdate>20110101</startdate><enddate>20110101</enddate><creator>NAKAMURA, Dai</creator><creator>GOTO, Takashi</creator><creator>ITO, Yoji</creator><creator>KIM, Hakusam</creator><creator>YAMASHITA, Satoshi</creator><creator>KAWAGUCHI, Takayuki</creator><creator>YAMASAKI, Shintaro</creator><creator>SUZUKI, Teruyuki</creator><general>The Mining and Materials Processing Institute of Japan</general><scope>7SR</scope><scope>8BQ</scope><scope>8FD</scope><scope>JG9</scope></search><sort><creationdate>20110101</creationdate><title>Basic Study on the Frost Heave Pressure of Rocks</title><author>NAKAMURA, Dai ; GOTO, Takashi ; ITO, Yoji ; KIM, Hakusam ; YAMASHITA, Satoshi ; KAWAGUCHI, Takayuki ; YAMASAKI, Shintaro ; SUZUKI, Teruyuki</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-j1560-d187f89c895ce0bb27ae1670d9b0192dfd913222cf03cdf01ca7a76d5399a05f3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng ; jpn</language><creationdate>2011</creationdate><topic>Frames</topic><topic>Frost</topic><topic>Frost Heave</topic><topic>Frost Heave Pressure</topic><topic>Frost Heave Rate</topic><topic>Heave</topic><topic>Ice Lens</topic><topic>Lenses</topic><topic>Rock</topic><topic>Rocks</topic><topic>Sandstone</topic><topic>Temperature Gradient</topic><topic>Tuff</topic><toplevel>online_resources</toplevel><creatorcontrib>NAKAMURA, Dai</creatorcontrib><creatorcontrib>GOTO, Takashi</creatorcontrib><creatorcontrib>ITO, Yoji</creatorcontrib><creatorcontrib>KIM, Hakusam</creatorcontrib><creatorcontrib>YAMASHITA, Satoshi</creatorcontrib><creatorcontrib>KAWAGUCHI, Takayuki</creatorcontrib><creatorcontrib>YAMASAKI, Shintaro</creatorcontrib><creatorcontrib>SUZUKI, Teruyuki</creatorcontrib><collection>Engineered Materials Abstracts</collection><collection>METADEX</collection><collection>Technology Research Database</collection><collection>Materials Research Database</collection><jtitle>Journal of MMIJ</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>NAKAMURA, Dai</au><au>GOTO, Takashi</au><au>ITO, Yoji</au><au>KIM, Hakusam</au><au>YAMASHITA, Satoshi</au><au>KAWAGUCHI, Takayuki</au><au>YAMASAKI, Shintaro</au><au>SUZUKI, Teruyuki</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Basic Study on the Frost Heave Pressure of Rocks: Dependence of the Maximum Frost Heave Pressure on Temperature</atitle><jtitle>Journal of MMIJ</jtitle><addtitle>J.MMIJ</addtitle><date>2011-01-01</date><risdate>2011</risdate><volume>127</volume><issue>8</issue><spage>485</spage><epage>496</epage><pages>485-496</pages><issn>1881-6118</issn><eissn>1884-0450</eissn><abstract>In this study, we attempted to measure frost heave pressure, i.e., the pressure that develops in the heat-flow direction when rocks are subject to frost heave and ice lenses grow. We used two kinds of rock samples: one was Ohya tuff, whose frost heave was already known to be high, and the other was Kimachi sandstone, whose frost heave was lower than that of the former. Ohya tuff and Kimachi sandstone, in which the occurrence of frost heave has previously been confirmed, were used as specimens. To conduct the experiment, we made original frost heave experiment equipment that was combined with a reaction frame and a load cell. The test results clearly showed that the maximum frost heave pressure did not depend on the kind of rock and was proportional to the temperature gradient. In addition, we clarified that the speed of the increase in pressure was proportional to the frost heave rate — the growth rate of the ice lens.</abstract><pub>The Mining and Materials Processing Institute of Japan</pub><doi>10.2473/journalofmmij.127.485</doi><tpages>12</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1881-6118 |
| ispartof | Journal of MMIJ, 2011/07/25, Vol.127(8), pp.485-496 |
| issn | 1881-6118 1884-0450 |
| language | eng ; jpn |
| recordid | cdi_proquest_miscellaneous_1022893420 |
| source | J-STAGE (Japan Science & Technology Information Aggregator, Electronic) Freely Available Titles - Japanese; EZB-FREE-00999 freely available EZB journals |
| subjects | Frames Frost Frost Heave Frost Heave Pressure Frost Heave Rate Heave Ice Lens Lenses Rock Rocks Sandstone Temperature Gradient Tuff |
| title | Basic Study on the Frost Heave Pressure of Rocks: Dependence of the Maximum Frost Heave Pressure on Temperature |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T08%3A48%3A13IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_jstag&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Basic%20Study%20on%20the%20Frost%20Heave%20Pressure%20of%20Rocks:%20Dependence%20of%20the%20Maximum%20Frost%20Heave%20Pressure%20on%20Temperature&rft.jtitle=Journal%20of%20MMIJ&rft.au=NAKAMURA,%20Dai&rft.date=2011-01-01&rft.volume=127&rft.issue=8&rft.spage=485&rft.epage=496&rft.pages=485-496&rft.issn=1881-6118&rft.eissn=1884-0450&rft_id=info:doi/10.2473/journalofmmij.127.485&rft_dat=%3Cproquest_jstag%3E1022893420%3C/proquest_jstag%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1022893420&rft_id=info:pmid/&rfr_iscdi=true |