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| 1 | 中德合作三江源区和甜水海地区多年冻土退化过程科学考察和研究进展显示文摘为准确了解青藏高原多年冻土退化过程及其环境效应,中国科学院寒区旱区环境与工程研究所和德国海德堡大学环境物理研究所共同组成科研小组,先后对我国三江源区、西昆仑甜水海地区进行了多年冻土退化过程的前期勘察研究工作.首次在人烟稀少的玉树-不冻泉沿线等地建立了3个长期综合观测研究站.在技术手段上,除应用常规的坑探、水土取样、水分现场观测、地面调查外,主要应用了最新的双天线、多回路探地雷达勘测技术,对不同地貌条件下的活动层结构特征、上限附近冻土结构、冷生组构等诸多方面进行了快速勘察,同时还进行了水分场分布规律、盐份迁移过程的初步研究.研究结果表明:地表景观特征对热质迁移规律、地温场具有重要影响;青藏高原新疆甜水海地区的低温(<-4℃)冻土与高原东部和腹地的高温(>-1℃)冻土在地质背景和地下冰发育情况等方面有所区别;甜水海地区生态环境在过去30多年的时间里已发生重大改变:地表植被发生大面积退化,地表普遍发生不同程度盐渍化;在该地区发现大量小型冻胀丘、石环等冰缘现象的存在.探地雷达勘察结果显示,地表地貌单元、植被分布、地表水分条件的变化均对多年冻土上限变化和地下冰的赋存产生重要影响. | 俞祁浩 Kurt Roth 金会军 潘喜才 Schiwek Philip Martin 盛煜 魏智 吴吉春 | 2006 | 冰川冻土2006，28，6： | 9 |
| 2 | Transfusion medicine and safety显示文摘 | Dodd R Kurt Roth W Ashford P | 2009 | Biologicals2009，37，2： | 1 |
| 3 | Ten questions concerning future buildings beyond zero energy and carbon neutrality显示文摘Architects and planners have been at the forefront of envisioning a future built environment for millennia. How ever,fragmental view s that emphasize one facet of the built environment,such as energy,environment,or groundbreaking technologies,often do not achieve expected outcomes. Buildings are responsible for approximately one-third of w orldw ide carbon emissions and account for about 40% of primary energy consumption in the U. S. In addition to achieving the very ambitious goal of reducing building-associated greenhouse gas emissions by75% by 2050,buildings must improve their functionality and performance to meet current and future human,societal,and environmental needs in a changing w orld. In this article,w e introduce a new framew ork to guide potential evolution of the building stock in the next century,based on greenhouse gas emissions as the common thread to investigate the potential implications of new design paradigms,innovative operational strategies,and disruptive technologies. This framew ork emphasizes integration of multidisciplinary know ledge,scalability for mainstream buildings,and proactive approaches considering constraints and unknow ns.The framew ork integrates the interrelated aspects of the built environment through a series of quantitative metrics that aim to improve environmental outcomes w hile optimizing building performance to achieve healthy,adaptive,and productive buildings. | Na Wang Patrick E. Phelan Jorge G onzalez Chioke Harris G regor P. Henze Robert Hutchinson Jared Langevin Mary Ann Lazarus Brent Nelson Chris Pyke Kurt Roth David Rouse Karma Sawyer Stephen Selkowitz 侯恩哲 | 2017 | 建筑节能2017，45，7： | 1 |
| 4 | Transfusion medicine and safety显示文摘 | DOdd R Kurt Roth W Ashford P | 2009 | Biologicals2009，37，2： | 1 |
| 5 | Transfusion medicine and safety显示文摘 | Dodd R Kurt Roth W Ashford P | 2009 | Biologicals2009，37，2： | 1 |
| 6 | Feasibility and efficacy of routine PCR screening of blood donations for hepatitis C virus, hepatitis B virus, and HIV-1 in a blood-bank setting显示文摘 | Willi Kurt Roth Marijke Weber Erhard Seifried | 1999 | The Lancet . 1999 (9150)1999，，9150： | 1 |
| 7 | Transfusion medicine and safety显示文摘 | Dodd R Kurt Roth W Ashford P | 2009 | Biologicals2009，37，2： | 1 |
| 8 | Heat pump water heaters显示文摘 | Zogg Robert Dieckmann John Roth Kurt | 2005 | ASHRAE Journal2005，47，3： | 1 |
| 9 | 一个秃冻胀丘的热及水文动力学——关于其形成的暗示(英)显示文摘Mud boils, classified as non-sorted circles, are a common patterned ground phenomenon of permafrost areas. They typically consist of a bare circle center of cryoturbated soil and are surrounded by vegetation on more stable soil. The objectives are to examine differences in seasonal hydrologic and thermal dynamic across this gradient of cryoturbation, i.e. the region below the organic border and the mud center. We installed instruments in a mud boil at a site close to Ny\|lesund, Spitsbergen, in September 1998. The bare soil circle center ranges about 1 m in diameter and is surrounded by a vegetated border consisting of a mixture of low vascular plants, mosses and lichens. Fine soil (>95% clay and silt) in the lower part of the profile is overlain by coarser grained material (silt and sand). The grain size distribution also suggests an upwelling of fine material in the center of the circle. Temperature and moisture sensors were installed over a vertical 1 m×1 m profile and hourly data recording started in September 1998. Surface irregularities, as well as variations of grain size and moisture, create a non\|uniform thermal and hydrologic dynamic. We qualitatively analyze this dynamic with respect to the mud boils physical stability. | Julia Boike~ 1,\ Alfred Wegener~ 1 ,\ Olaf Ippisch~ 2 ,\ Kurt Roth~ 2 (1. Institute for Polar and Marine Research, Potsdam, Germany 2. Institute for Environmental Physics, University of Heidelberg, Heidelberg, Germany) | 2002 | 冰川冻土2002，24，5： | 0 |
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