2012-2016年基于文献计量的全球冻土研究发展态势分析
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摘要
冻土是冰冻圈的重要组成部分,其对全球变暖敏感且对工程稳定性影响显著,近年来全球科学家更多地关注这一研究领域。作为世界冻土大区的中国,对冻土学科的发展和动态尤其重视。本文基于文献计量的方法,对近五年(2012-2016)冻土学领域发表的SCI(E)/CPCI收录论文进行统计分析,得到该领域在全球的研究力量分布。同时,分别从冻土工程、冻土力学、冻土环境、冻土物理这四个方向加以区分,得到其不同机构与科学家论文发表情况。从论文产出的角度,宏观地反映了冻土科学在这五年中的发展脉络与国际影响力。这一工作可为全面了解近期该领域的研究发展动态提供数据参考。
Study of frozen soil(including permafrost) gradually attracted the attention of global scientists, because frozen soil is an important component of the cryosphere, and it is sensitive to global warming and has the most effect on the stability of engineering. China, as one of the largest permafrost region, pays special attention to the development tendency of geocryology. Using the well-established bibliometrical analysis method, the papers published in the field of frozen soil(including permafrost) have been statistically analyzed, included in SCI(E)/CPCI bases from 2012-2016, and determined the order of scientific research strength in this field. The published papers can divided as frozen soil engineering, frozen soil mechanics, permafrost environment, and frozen soil physics. The results will present the development tendency and international influence of permafrost science during the past five years. It is useful for future development in this field.
Study of frozen soil(including permafrost) gradually attracted the attention of global scientists, because frozen soil is an important component of the cryosphere, and it is sensitive to global warming and has the most effect on the stability of engineering. China, as one of the largest permafrost region, pays special attention to the development tendency of geocryology. Using the well-established bibliometrical analysis method, the papers published in the field of frozen soil(including permafrost) have been statistically analyzed, included in SCI(E)/CPCI bases from 2012-2016, and determined the order of scientific research strength in this field. The published papers can divided as frozen soil engineering, frozen soil mechanics, permafrost environment, and frozen soil physics. The results will present the development tendency and international influence of permafrost science during the past five years. It is useful for future development in this field.
引文
[1] Zhou Youwu,Guo Dongxin,Qiu Guoqing,et al.Geocryology in China[M].Beijing:Science Press,2000.[周幼吾,郭东信,邱国庆,等.中国冻土[M].北京:科学出版社,2000.]
[2] Li Qian,Chen Haishan.Variation of seasonal frozen soil in East China and their association with monsoon activity under the background of global warming[J].Climate Change Research Letters,2013,2:47-53.[李倩,陈海山.全球变暖背景下中国东部季节性冻土的变化特征及其与季风活动的可能联系[J].气候变化研究快报,2013,2:47-53.]
[3] Cheng Guodong.Review and prospect of regional geocryology in China[J].Journal of Geophysical Research,1988,10(3):296-299.[程国栋.中国区域冻土研究的回顾和展望[J].冰川冻土,1988,10(3):296-299.]
[4] Zhang Tingjun.Represents an important milestone in the research of frozen soil in China[J].Journal of Geophysical Research,2002,24(3):331-334.[张廷军.代表中国冻土学研究的一个重要里程碑[J].冰川冻土,2002,24(3):331-334.]
[5] Sun Hong,Niu Fujun,Zhang Kaijian,et al.Seismic behaviors of soil slope in permafrost regions using a large-scale shaking table[J].Landslides,2017,14(4):1513-1520.
[6] Cheng Guodong,Wu Tonghua.Responses of permafrost to climate change and their environmental significance,Qinghai-Tibet Plateau[J].Journal of Geophysical Research:Earth Surface,2007,112(F2).
[7] Wu Qingbai,Zhang Tingjun.Recent permafrost warming on the Qinghai-Tibetan plateau[J].Journal of Geophysical Research-Atmospheres,2008,113(D13).
[8] Wu Qingbai,Yu Wenbing,Jin Huijun.No protection of permafrost due to desertification on the Qinghai Tibet Plateau[J].Scientific reports,2017,7(1):1544.
[9] Li Xin,Cheng Guodong,Jin Huijun,et al.Cryospheric change in China[J].Global and Planetary Change,2008,62(3/4):210-218.
[10] Wu Qingbai,Zhang Tingjun.Changes in active layer thickness over the Qinghai-Tibetan Plateau from 1995 to 2007[J].Journal of Geophysical Research-Atmospheres,2010,115(D9).
[11] Ling Feng,Wu Qingbai.Numerical simulation of influence of thermokarst lake horizontal expansion rate on talik development beneath thermokarst lakes on Qinghai-Tibet Plateau[J].Journal of Glaciology and Geocryology,2017,39(2):328-335.[令锋,吴青柏.青藏高原热融湖横向扩张速率对湖下融区发展影响的数值模拟[J].冰川冻土,2017,39(2):328-335.]
[12] Zhang Xuanwen,Yang Li,Liu Xiaohong,et al.Study of the difference in climate response of Dahurian Larch and Pinus sylvestris growth in the north Great Higgnan Mountains of permafrost regions,Northeast China[J].Journal of Glaciology and Geocryology,2017,39(1):165-174.[张轩文,杨丽,刘晓宏,等.大兴安岭北部多年冻土区落叶松和樟子松生长的气候响应差异研究[J].冰川冻土,2017,39(1):165-174.]
[13] Xu Xiaoming,Wu Qingbai,Zhang Zhongqiong.Responses of active layer thickness on the Qinghai-Tibet Plateau to climate change[J].Journal of Glaciology and Geocryology,2017,39(1):1-8.[徐晓明,吴青柏,张中琼.青藏高原多年冻土活动层厚度对气候变化的响应[J].冰川冻土,2017,39(1):1-8.]
[14] Cui Lei,Liu Wei,Yan Lei,et al.Development of a text mining system based on the co-occurrence of bibliographic items in literature databases[J].New Technology of Library and Information Service,2008,24(8):70-75.[崔雷,刘伟,闫雷,等.文献数据库中书目信息共现挖掘系统的开发[J].数据分析与知识发现,2008,24(8):70-75.]
[15] Lin Changyan,Li Yanping,Shu Lixia,et al.Literature metrology analysis for status and trends of biomedical engineering in China[J].Beijing Biomedical Engineering,2010,29(6):608-612.[蔺嫦燕,李砚平,舒丽霞,等.中国生物医学工程学科发展态势的文献计量学分析[J].北京生物医学工程,2010,29(6):608-612.]
[16] Liu Hao,Zhang Zhiqiang,Fan Shaoping.Bibliometrical analysis on development tendency of informatics[J].Information Research,2017,233(3):102-110.[刘昊,张志强,范少萍.信息学学科发展态势文献计量分析[J].情报探索,2017,233(3):102-110.]
[17] Mu Yafeng,Du Pingping,Qi Maitu,et al.Research on the trend of discipline development based on citation analysis[J].Journal of Modern Information.2017,37(3):126-131.[穆亚凤,都平平,齐迈图,等.基于引文分析工具的学科发展态势研究[J].现代情报,2017,37(3):126-131.]
[18] Feng Yun,Zheng Junwei.An analysis of status and trends of the international remote sensing science on bibliometrics[J].Remote Sensing Technology and Application,2005,20(5):70-74.[冯筠,郑军卫.基于文献计量学的国际遥感学科发展态势分析[J].遥感技术与应用,2005,20(5):70-74.]
[19] Qiu Guoqing,Liu Jingren,Liu Hongxu.Geocrylolgical glossary[M].Lanzhou:Gansu Science and Technology Press,1994.[邱国庆,刘经仁,刘鸿绪.冻土学辞典:汉、 英、 俄对照[M].兰州:甘肃科学技术出版社,1994.]
(1)*(星号):任何字符组,包括空字符,可用来检索词语的单复数与动名词等的变化形式。如:Gelisol*检索时同时可检索到Gelisol和Gelisols。
(2)“”(双引号):词组中单词顺序的固定,可用来检索固定搭配词组。如"frozen soil*"只能同时出现且位置不变才可被检索出来。
[2] Li Qian,Chen Haishan.Variation of seasonal frozen soil in East China and their association with monsoon activity under the background of global warming[J].Climate Change Research Letters,2013,2:47-53.[李倩,陈海山.全球变暖背景下中国东部季节性冻土的变化特征及其与季风活动的可能联系[J].气候变化研究快报,2013,2:47-53.]
[3] Cheng Guodong.Review and prospect of regional geocryology in China[J].Journal of Geophysical Research,1988,10(3):296-299.[程国栋.中国区域冻土研究的回顾和展望[J].冰川冻土,1988,10(3):296-299.]
[4] Zhang Tingjun.Represents an important milestone in the research of frozen soil in China[J].Journal of Geophysical Research,2002,24(3):331-334.[张廷军.代表中国冻土学研究的一个重要里程碑[J].冰川冻土,2002,24(3):331-334.]
[5] Sun Hong,Niu Fujun,Zhang Kaijian,et al.Seismic behaviors of soil slope in permafrost regions using a large-scale shaking table[J].Landslides,2017,14(4):1513-1520.
[6] Cheng Guodong,Wu Tonghua.Responses of permafrost to climate change and their environmental significance,Qinghai-Tibet Plateau[J].Journal of Geophysical Research:Earth Surface,2007,112(F2).
[7] Wu Qingbai,Zhang Tingjun.Recent permafrost warming on the Qinghai-Tibetan plateau[J].Journal of Geophysical Research-Atmospheres,2008,113(D13).
[8] Wu Qingbai,Yu Wenbing,Jin Huijun.No protection of permafrost due to desertification on the Qinghai Tibet Plateau[J].Scientific reports,2017,7(1):1544.
[9] Li Xin,Cheng Guodong,Jin Huijun,et al.Cryospheric change in China[J].Global and Planetary Change,2008,62(3/4):210-218.
[10] Wu Qingbai,Zhang Tingjun.Changes in active layer thickness over the Qinghai-Tibetan Plateau from 1995 to 2007[J].Journal of Geophysical Research-Atmospheres,2010,115(D9).
[11] Ling Feng,Wu Qingbai.Numerical simulation of influence of thermokarst lake horizontal expansion rate on talik development beneath thermokarst lakes on Qinghai-Tibet Plateau[J].Journal of Glaciology and Geocryology,2017,39(2):328-335.[令锋,吴青柏.青藏高原热融湖横向扩张速率对湖下融区发展影响的数值模拟[J].冰川冻土,2017,39(2):328-335.]
[12] Zhang Xuanwen,Yang Li,Liu Xiaohong,et al.Study of the difference in climate response of Dahurian Larch and Pinus sylvestris growth in the north Great Higgnan Mountains of permafrost regions,Northeast China[J].Journal of Glaciology and Geocryology,2017,39(1):165-174.[张轩文,杨丽,刘晓宏,等.大兴安岭北部多年冻土区落叶松和樟子松生长的气候响应差异研究[J].冰川冻土,2017,39(1):165-174.]
[13] Xu Xiaoming,Wu Qingbai,Zhang Zhongqiong.Responses of active layer thickness on the Qinghai-Tibet Plateau to climate change[J].Journal of Glaciology and Geocryology,2017,39(1):1-8.[徐晓明,吴青柏,张中琼.青藏高原多年冻土活动层厚度对气候变化的响应[J].冰川冻土,2017,39(1):1-8.]
[14] Cui Lei,Liu Wei,Yan Lei,et al.Development of a text mining system based on the co-occurrence of bibliographic items in literature databases[J].New Technology of Library and Information Service,2008,24(8):70-75.[崔雷,刘伟,闫雷,等.文献数据库中书目信息共现挖掘系统的开发[J].数据分析与知识发现,2008,24(8):70-75.]
[15] Lin Changyan,Li Yanping,Shu Lixia,et al.Literature metrology analysis for status and trends of biomedical engineering in China[J].Beijing Biomedical Engineering,2010,29(6):608-612.[蔺嫦燕,李砚平,舒丽霞,等.中国生物医学工程学科发展态势的文献计量学分析[J].北京生物医学工程,2010,29(6):608-612.]
[16] Liu Hao,Zhang Zhiqiang,Fan Shaoping.Bibliometrical analysis on development tendency of informatics[J].Information Research,2017,233(3):102-110.[刘昊,张志强,范少萍.信息学学科发展态势文献计量分析[J].情报探索,2017,233(3):102-110.]
[17] Mu Yafeng,Du Pingping,Qi Maitu,et al.Research on the trend of discipline development based on citation analysis[J].Journal of Modern Information.2017,37(3):126-131.[穆亚凤,都平平,齐迈图,等.基于引文分析工具的学科发展态势研究[J].现代情报,2017,37(3):126-131.]
[18] Feng Yun,Zheng Junwei.An analysis of status and trends of the international remote sensing science on bibliometrics[J].Remote Sensing Technology and Application,2005,20(5):70-74.[冯筠,郑军卫.基于文献计量学的国际遥感学科发展态势分析[J].遥感技术与应用,2005,20(5):70-74.]
[19] Qiu Guoqing,Liu Jingren,Liu Hongxu.Geocrylolgical glossary[M].Lanzhou:Gansu Science and Technology Press,1994.[邱国庆,刘经仁,刘鸿绪.冻土学辞典:汉、 英、 俄对照[M].兰州:甘肃科学技术出版社,1994.]
(1)*(星号):任何字符组,包括空字符,可用来检索词语的单复数与动名词等的变化形式。如:Gelisol*检索时同时可检索到Gelisol和Gelisols。
(2)“”(双引号):词组中单词顺序的固定,可用来检索固定搭配词组。如"frozen soil*"只能同时出现且位置不变才可被检索出来。
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