1![This article was originally published in a journal published by Elsevier, and the attached copy is provided by Elsevier for the author’s benefit and for the benefit of the author’s institution, for non-commercial res This article was originally published in a journal published by Elsevier, and the attached copy is provided by Elsevier for the author’s benefit and for the benefit of the author’s institution, for non-commercial res](https://www.pdfsearch.io/img/5d77bed77f43b3a239a2fb4fd558001c.jpg) | Add to Reading ListSource URL: physics.lnu.edu.uaLanguage: English - Date: 2014-07-22 04:23:00
|
---|
2![Scottish Curling-Ice Group WHY DO CURLING STONES CURL The study of why curling stones curl is not new. Many theories have been suggested by highly qualified individuals and many have been flawed, while others have looked Scottish Curling-Ice Group WHY DO CURLING STONES CURL The study of why curling stones curl is not new. Many theories have been suggested by highly qualified individuals and many have been flawed, while others have looked](https://www.pdfsearch.io/img/0d4ce5dceef1094b72827da5bd4956aa.jpg) | Add to Reading ListSource URL: www.scottishcurlingicegroup.orgLanguage: English - Date: 2011-02-26 12:42:00
|
---|
3![Hydrous mineral formation reaction between amorphous forsterite and water vapor in protoplanetary disks D. Yamamoto1, S. Tachibana1, H.Nagahara2 , K. Ozawa2 and A. Tsuchiyama3 1 Department of Natural History Science of H Hydrous mineral formation reaction between amorphous forsterite and water vapor in protoplanetary disks D. Yamamoto1, S. Tachibana1, H.Nagahara2 , K. Ozawa2 and A. Tsuchiyama3 1 Department of Natural History Science of H](https://www.pdfsearch.io/img/0b4112492676bc6fbd215386748d617b.jpg) | Add to Reading ListSource URL: www.nipr.ac.jpLanguage: English - Date: 2014-11-16 09:41:57
|
---|
4![Atmos. Chem. Phys., 9, 965–971, 2009 www.atmos-chem-phys.net[removed]/ © Author(s[removed]This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric Atmos. Chem. Phys., 9, 965–971, 2009 www.atmos-chem-phys.net[removed]/ © Author(s[removed]This work is distributed under the Creative Commons Attribution 3.0 License. Atmospheric](https://www.pdfsearch.io/img/d91fb18fad65cb9c9af37542d4af2dde.jpg) | Add to Reading ListSource URL: www.ace.uwaterloo.caLanguage: English - Date: 2009-02-06 15:43:48
|
---|
5![PROOF COPY [BP10610] 133839PRB PHYSICAL REVIEW B 78, 1 共2008兲 2 Simulation of nanodiamond and nanographite formation from molten carbon PROOF COPY [BP10610] 133839PRB PHYSICAL REVIEW B 78, 1 共2008兲 2 Simulation of nanodiamond and nanographite formation from molten carbon](https://www.pdfsearch.io/img/60d8c46315922ca251c81a4b800a06c2.jpg) | Add to Reading ListSource URL: phjoan23.technion.ac.ilLanguage: English - Date: 2008-10-29 05:38:06
|
---|
6![egu_logo_without_circle_grey egu_logo_without_circle_grey](https://www.pdfsearch.io/img/46494a01212d8e390e69ce308ae0c91b.jpg) | Add to Reading ListSource URL: www.atmos-chem-phys.netLanguage: English - Date: 2013-12-09 08:30:17
|
---|
7![review article The relationship between liquid, review article The relationship between liquid,](https://www.pdfsearch.io/img/d6768873aaebc83c7e6731262d7a8b9b.jpg) | Add to Reading ListSource URL: polymer.bu.eduLanguage: English - Date: 2002-10-01 11:52:32
|
---|
8![review article The relationship between liquid, review article The relationship between liquid,](https://www.pdfsearch.io/img/6d7c759fddb475ba1ab6a2d390993083.jpg) | Add to Reading ListSource URL: www.nims.jpLanguage: English - Date: 2002-10-18 07:55:36
|
---|
9![Available online at www.sciencedirect.com R Available online at www.sciencedirect.com R](https://www.pdfsearch.io/img/86b8ddf3bd156c1b6d6cefad794577a8.jpg) | Add to Reading ListSource URL: www.ifa.hawaii.eduLanguage: English - Date: 2006-03-19 18:10:03
|
---|
10![letters to nature the target range for DRAM applications (1–5 ϫ 10 Ϫ 7 A cm Ϫ 2 ). At this composition, we find er ¼ 62:5 and the FOM is 24.3 C cm−2. letters to nature the target range for DRAM applications (1–5 ϫ 10 Ϫ 7 A cm Ϫ 2 ). At this composition, we find er ¼ 62:5 and the FOM is 24.3 C cm−2.](https://www.pdfsearch.io/img/b68d97f392c455ee36d92654ff065b7c.jpg) | Add to Reading ListSource URL: www.nims.go.jpLanguage: English - Date: 2002-10-18 07:55:36
|
---|