Huang et al. reply
Replying to F. M. Richter Nature472, 10.1038/nature09954 (2011) In our Letter 1 , we showed that the phenomenon of isotope fractionation in silicate melts by thermal diffusion, first reported in 1998 (ref. 2 ), can be characterised by a parameter Δ S T that is independent of temperature and composit...
Gespeichert in:
| Veröffentlicht in: | Nature (London) 2011-04, Vol.472 (7341), p.E2-E3 |
|---|---|
| Hauptverfasser: | , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | E3 |
|---|---|
| container_issue | 7341 |
| container_start_page | E2 |
| container_title | Nature (London) |
| container_volume | 472 |
| creator | Huang, F. Chakraborty, P. Lundstrom, C. C. Holmden, C. Glessner, J. J. G. Kieffer, S. W. Lesher, C. E. |
| description | Replying to
F. M. Richter
Nature472, 10.1038/nature09954 (2011)
In our Letter
1
, we showed that the phenomenon of isotope fractionation in silicate melts by thermal diffusion, first reported in 1998 (ref.
2
), can be characterised by a parameter Δ
S
T
that is independent of temperature and composition. (Here Δ
S
T
is the difference in the Soret coefficient,
S
T
, between isotopes of a diffusing element.) Richter
3
questioned this finding by plotting Mg isotope ratio versus temperature data (figure 1 in ref.
3
) for a subset of experiments from figure 3f of ref.
1
. |
| doi_str_mv | 10.1038/nature09955 |
| format | Article |
| fullrecord | <record><control><sourceid>gale_cross</sourceid><recordid>TN_cdi_gale_infotracmisc_A254404190</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A254404190</galeid><sourcerecordid>A254404190</sourcerecordid><originalsourceid>FETCH-LOGICAL-c3875-f070dab1d36da83a28e966e896648978b480c5ac7619deb7cd708c5c3d3850263</originalsourceid><addsrcrecordid>eNp10U1Lw0AQBuBFFKzVi_6BoifR1NnsZ46hqC0UBa14XLabTUhJk7qbgP33rtRDC5GBGRiemcuL0BWGMQYiH2rdds5CkjB2hAaYCh5RLsUxGgDEMgJJ-Ck6834FAAwLOkCX007Xxci2I12NR85uqu05Osl15e3F3xyij6fHxWQazV-fZ5N0HhkiBYtyEJDpJc4Iz7QkOpY24dzK0KhMhFxSCYZpIzhOMrsUJhMgDTMkI5JBzMkQ3ez-FrqyqqzzpnXarEtvVBozSoHiBIKKelRha-t01dQ2L8P6wF_3eLMpv9Q-GvegUJldl6b36-3BQTCt_W4L3XmvZu9vh_buf5suPicvvdq4xntnc7Vx5Vq7rcKgfkNVe6EGfb_TPqi6sE6tms7VIaZe_gNn4pzQ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>Huang et al. reply</title><source>Nature</source><source>Springer Nature - Complete Springer Journals</source><creator>Huang, F. ; Chakraborty, P. ; Lundstrom, C. C. ; Holmden, C. ; Glessner, J. J. G. ; Kieffer, S. W. ; Lesher, C. E.</creator><creatorcontrib>Huang, F. ; Chakraborty, P. ; Lundstrom, C. C. ; Holmden, C. ; Glessner, J. J. G. ; Kieffer, S. W. ; Lesher, C. E.</creatorcontrib><description>Replying to
F. M. Richter
Nature472, 10.1038/nature09954 (2011)
In our Letter
1
, we showed that the phenomenon of isotope fractionation in silicate melts by thermal diffusion, first reported in 1998 (ref.
2
), can be characterised by a parameter Δ
S
T
that is independent of temperature and composition. (Here Δ
S
T
is the difference in the Soret coefficient,
S
T
, between isotopes of a diffusing element.) Richter
3
questioned this finding by plotting Mg isotope ratio versus temperature data (figure 1 in ref.
3
) for a subset of experiments from figure 3f of ref.
1
.</description><identifier>ISSN: 0028-0836</identifier><identifier>EISSN: 1476-4687</identifier><identifier>DOI: 10.1038/nature09955</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>704/2151/213 ; brief-communications-arising ; Humanities and Social Sciences ; Isotopes ; multidisciplinary ; Science ; Science (multidisciplinary) ; Silicates ; Thermal diffusivity</subject><ispartof>Nature (London), 2011-04, Vol.472 (7341), p.E2-E3</ispartof><rights>Springer Nature Limited 2011</rights><rights>COPYRIGHT 2011 Nature Publishing Group</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3875-f070dab1d36da83a28e966e896648978b480c5ac7619deb7cd708c5c3d3850263</citedby><cites>FETCH-LOGICAL-c3875-f070dab1d36da83a28e966e896648978b480c5ac7619deb7cd708c5c3d3850263</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1038/nature09955$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1038/nature09955$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51298</link.rule.ids></links><search><creatorcontrib>Huang, F.</creatorcontrib><creatorcontrib>Chakraborty, P.</creatorcontrib><creatorcontrib>Lundstrom, C. C.</creatorcontrib><creatorcontrib>Holmden, C.</creatorcontrib><creatorcontrib>Glessner, J. J. G.</creatorcontrib><creatorcontrib>Kieffer, S. W.</creatorcontrib><creatorcontrib>Lesher, C. E.</creatorcontrib><title>Huang et al. reply</title><title>Nature (London)</title><addtitle>Nature</addtitle><description>Replying to
F. M. Richter
Nature472, 10.1038/nature09954 (2011)
In our Letter
1
, we showed that the phenomenon of isotope fractionation in silicate melts by thermal diffusion, first reported in 1998 (ref.
2
), can be characterised by a parameter Δ
S
T
that is independent of temperature and composition. (Here Δ
S
T
is the difference in the Soret coefficient,
S
T
, between isotopes of a diffusing element.) Richter
3
questioned this finding by plotting Mg isotope ratio versus temperature data (figure 1 in ref.
3
) for a subset of experiments from figure 3f of ref.
1
.</description><subject>704/2151/213</subject><subject>brief-communications-arising</subject><subject>Humanities and Social Sciences</subject><subject>Isotopes</subject><subject>multidisciplinary</subject><subject>Science</subject><subject>Science (multidisciplinary)</subject><subject>Silicates</subject><subject>Thermal diffusivity</subject><issn>0028-0836</issn><issn>1476-4687</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2011</creationdate><recordtype>article</recordtype><recordid>eNp10U1Lw0AQBuBFFKzVi_6BoifR1NnsZ46hqC0UBa14XLabTUhJk7qbgP33rtRDC5GBGRiemcuL0BWGMQYiH2rdds5CkjB2hAaYCh5RLsUxGgDEMgJJ-Ck6834FAAwLOkCX007Xxci2I12NR85uqu05Osl15e3F3xyij6fHxWQazV-fZ5N0HhkiBYtyEJDpJc4Iz7QkOpY24dzK0KhMhFxSCYZpIzhOMrsUJhMgDTMkI5JBzMkQ3ez-FrqyqqzzpnXarEtvVBozSoHiBIKKelRha-t01dQ2L8P6wF_3eLMpv9Q-GvegUJldl6b36-3BQTCt_W4L3XmvZu9vh_buf5suPicvvdq4xntnc7Vx5Vq7rcKgfkNVe6EGfb_TPqi6sE6tms7VIaZe_gNn4pzQ</recordid><startdate>20110407</startdate><enddate>20110407</enddate><creator>Huang, F.</creator><creator>Chakraborty, P.</creator><creator>Lundstrom, C. C.</creator><creator>Holmden, C.</creator><creator>Glessner, J. J. G.</creator><creator>Kieffer, S. W.</creator><creator>Lesher, C. E.</creator><general>Nature Publishing Group UK</general><general>Nature Publishing Group</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ATWCN</scope></search><sort><creationdate>20110407</creationdate><title>Huang et al. reply</title><author>Huang, F. ; Chakraborty, P. ; Lundstrom, C. C. ; Holmden, C. ; Glessner, J. J. G. ; Kieffer, S. W. ; Lesher, C. E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3875-f070dab1d36da83a28e966e896648978b480c5ac7619deb7cd708c5c3d3850263</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2011</creationdate><topic>704/2151/213</topic><topic>brief-communications-arising</topic><topic>Humanities and Social Sciences</topic><topic>Isotopes</topic><topic>multidisciplinary</topic><topic>Science</topic><topic>Science (multidisciplinary)</topic><topic>Silicates</topic><topic>Thermal diffusivity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Huang, F.</creatorcontrib><creatorcontrib>Chakraborty, P.</creatorcontrib><creatorcontrib>Lundstrom, C. C.</creatorcontrib><creatorcontrib>Holmden, C.</creatorcontrib><creatorcontrib>Glessner, J. J. G.</creatorcontrib><creatorcontrib>Kieffer, S. W.</creatorcontrib><creatorcontrib>Lesher, C. E.</creatorcontrib><collection>CrossRef</collection><collection>Gale In Context: Middle School</collection><jtitle>Nature (London)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Huang, F.</au><au>Chakraborty, P.</au><au>Lundstrom, C. C.</au><au>Holmden, C.</au><au>Glessner, J. J. G.</au><au>Kieffer, S. W.</au><au>Lesher, C. E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Huang et al. reply</atitle><jtitle>Nature (London)</jtitle><stitle>Nature</stitle><date>2011-04-07</date><risdate>2011</risdate><volume>472</volume><issue>7341</issue><spage>E2</spage><epage>E3</epage><pages>E2-E3</pages><issn>0028-0836</issn><eissn>1476-4687</eissn><abstract>Replying to
F. M. Richter
Nature472, 10.1038/nature09954 (2011)
In our Letter
1
, we showed that the phenomenon of isotope fractionation in silicate melts by thermal diffusion, first reported in 1998 (ref.
2
), can be characterised by a parameter Δ
S
T
that is independent of temperature and composition. (Here Δ
S
T
is the difference in the Soret coefficient,
S
T
, between isotopes of a diffusing element.) Richter
3
questioned this finding by plotting Mg isotope ratio versus temperature data (figure 1 in ref.
3
) for a subset of experiments from figure 3f of ref.
1
.</abstract><cop>London</cop><pub>Nature Publishing Group UK</pub><doi>10.1038/nature09955</doi><tpages>1</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0028-0836 |
| ispartof | Nature (London), 2011-04, Vol.472 (7341), p.E2-E3 |
| issn | 0028-0836 1476-4687 |
| language | eng |
| recordid | cdi_gale_infotracmisc_A254404190 |
| source | Nature; Springer Nature - Complete Springer Journals |
| subjects | 704/2151/213 brief-communications-arising Humanities and Social Sciences Isotopes multidisciplinary Science Science (multidisciplinary) Silicates Thermal diffusivity |
| title | Huang et al. reply |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-22T08%3A26%3A28IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Huang%20et%20al.%20reply&rft.jtitle=Nature%20(London)&rft.au=Huang,%20F.&rft.date=2011-04-07&rft.volume=472&rft.issue=7341&rft.spage=E2&rft.epage=E3&rft.pages=E2-E3&rft.issn=0028-0836&rft.eissn=1476-4687&rft_id=info:doi/10.1038/nature09955&rft_dat=%3Cgale_cross%3EA254404190%3C/gale_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_galeid=A254404190&rfr_iscdi=true |