|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | Thermal regimes and degradation modes of permafrost along the Qinghai-Tibet Highway显示文摘Permafrost on the Qinghai-Tibet Plateau (QTP) is widespread, thin, and thermally unstable. Under a warming climate during the past few decades, it has been degrading extensively with generally rising ground temperatures, the deepening of the maximum summer thaw, and with lessening of the winter frost penetration. The permafrost has degraded downward, upward and laterally. Permafrost has thinned or, in some areas, has totally disappeared. The modes of permafrost degradation have great significance in geocryology, in cold regions engineering and in cold regions environmental management. Permafrost in the interior of the QTP is well represented along the Qing-hai-Tibet Highway (QTH), which crosses the Plateau through north to south and traverses 560 km of permafrost-impacted ground. Horizontally, the degradation of permafrost occurs more visibly in the sporadic permafrost zone in the vicinity of the lower limit of permafrost (LLP), along the margins of taliks, and around permafrost islands. Downward degradation develops when the maximum depth of seasonal thaw exceeds the maximum depth of seasonal frost, and it generally results in the formation of a layered talik disconnecting the permafrost from the seasonal frost layer. The downward degrada- tion is divided into four stages: 1) initial degradation, 2) accelerated degradation, 3) layered talik and 4) finally the conversion of permafrost to seasonally frozen ground (SFG). The upward degradation occurs when the geothermal gradient in permafrost drops to less than the geothermal gradients in the underlying thawed soil layers. Three types of permafrost temperature curves (stable, degrading, and phase-changing transitory permafrost) illustrate these modes. Although strong differentiations in local conditions and permafrost types exist, the various combinations of the three degradation modes will ultimately transform permafrost into SFG. Along the QTH, the downward degradation has been proceeding at annual rates of 6 to 25 cm, upward degradation at 12 to 30 cm, and lateral degradation in the sporadic permafrost zone at 62 to 94 cm during the last quarter century. These rates exceed the 4 cm per year for the past 20 years reported for the discontinuous permafrost zone in subarctic Alaska, the 3 to 7 cm per year reported in Mongolia, and that of the thaw-stable permafrost in subarctic Yakutia and Arctic Alaska. | JIN Huijun ZHAO Lin WANG Shaoling JIN Rui | 2006 | Science China Earth Sciences2006，49，11： | 50 |
| 2 | Thawing and freezing processes of active layer in Wudaoliang region of Tibetan Plateau显示文摘The interaction between permafrost and atmosphere is accomplished through transfer of heat and moisture in the overlay active layer. Thus, the research on the thermal and hydrodynamics of active layer during the thawing and freezing processes was considered a key to revealing the heat and moisture exchanges between permafrost and atmosphere. The monitoring and research on active layer were conducted because permafrost occupies about two thirds of the total area of the Tibetan Plateau. Based on the analysis of the ground temperature data and soil moisture data of monitoring near the Wudaoliang region of the Tibetan Plateau, the thawing and freezing processes of active layer were divided into four stages, i.e. summer thawing stage (ST), autumn freezing stage (AF), winter cooling stage (WC) and spring warming stage (SW). Coupled heat and water flow is much more complicated in ST and AF, and more amount of water is migrating in these two stages. Heat is transferred mainly via conductive heat flow in the | Lin Zhao Guodong Cheng Shuxun Li Xinmin Zhao Shaoling Wang | 2000 | Chinese Science Bulletin2000，45，23： | 31 |
| 3 | Spatiotemporal variability of permafrost degradation on the Qinghai-Tibet Plateau显示文摘Based on data from six meteorological stations in the permafrost regions, 60 boreholes for long-term monitoring of permafrost temperatures, and 710 hand-dug pits and shallow boreholes on the Qinghai-Tibet Plateau (QTP), the spatiotemporal variability of permafrost degradation was closely examined in relation to the rates of changes in air, surface, and ground temperatures. The de-cadal averages and increases in the mean annual air temperatures (MAATs) from 1961-2010 were the largest and most persistent during the last century. MAATs rose by 1.3℃, with an average increase rate of 0.03℃/yr. The average of mean annual ground surface temperatures (MAGSTs) increased by 1.3℃ at an average rate of 0.03℃/yr. The rates of changes in ground temperatures were -0.01 to 0.07℃/yr. The rates of changes in the depths of the permafrost table were -1 to +10 cm/yr. The areal extent of permafrost on the QTP shrank from about 1.50×106 km2 in 1975 to about 1.26×106 km2 in 2006. About 60% of the shrinkage in area of permafrost occurred during the period from 1996 to 2006. Due to increasing air temperature since the late 1980s, warm (>-1℃) permafrost has started to degrade, and the degradation has gradually expanded to the zones of transitory (-1 to -2℃) and cold (<-2℃) permafrost. Permafrost on the southern and southeastern plateau degrades more markedly. It is projected that the degradation of permafrost is likely to accelerate, and substantial changes in the distributive features and thermal regimes of permafrost should be anticipated. However, regarding the relationships between degrading permafrost and the degradation of rangelands, it is still too early to draw reliable conclusions due to inadequate scientific criteria and evidence. | HuiJun Jin DongLiang Luo ShaoLing Wang LanZhi Lv JiChun Wu | 2011 | Research in Cold and Arid Regions2011，3，4： | 16 |
| 4 | Monitoring of frozen soil hydrology in macro-scale in the Qinghai-Xizang Plateau显示文摘Monitoring of frozen soil hydrology in macro-scale was performed by Chinese and Japanese scientists from 1997 to 1998. Quality measured data were obtained. Measured data on soil moisture and temperature are preliminarily analyzed. Based on profiles of soil temperature and moisture in individual measured sites, intra-annual freezing and melting process of soil is discussed. Maximum frozen and thawed depths and frozen days in various depths are estimated. The work emphasized the spatial distribution on soil temperature and moisture in macro-scale and the effect of topography on conditions of soil water and heat. | Yongjian Ding Baisheng Ye Shiying Liu Yongping Shen Shaoling Wang Meixie Yang | 2000 | Chinese Science Bulletin2000，45，12： | 13 |
| 5 | Evolution of permafrost in China during the last 20 ka显示文摘The formation and evolution of permafrost in China during the last 20 ka were reconstructed on the basis of large amount of paleo-permafrost remains and paleo-periglacial evidence, as well as paleo-glacial landforms, paleo-flora and paleofauna records. The results indicate that, during the local Last Glacial Maximum(LLGM) or local Last Permafrost Maximum(LLPMax), the extent of permafrost of China reached 5.3×106-5.4×106 km2, or thrice that of today, but permafrost shrank to only0.80×106-0.85×106 km2, or 50% that of present, during the local Holocene Megathermal Period(LHMP), or the local Last Permafrost Minimum(LLPMin). On the basis of the dating of periglacial remains and their distributive features, the extent of permafrost in China was delineated for the two periods of LLGM(LLPMax) and LHMP(LLPMin), and the evolution of permafrost in China was divided into seven periods as follows:(1) LLGM in Late Pleistocene(ca. 20000 to 13000-10800 a BP)with extensive evidence for the presence of intensive ice-wedge expansion for outlining its LLPMax extent;(2) A period of dramatically changing climate during the early Holocene(10800 to 8500-7000 a BP) when permafrost remained relatively stable but with a general trend of shrinking areal extent;(3) The LHMP in the Mid-Holocene(8500-7000 to 4000-3000 a BP)when permafrost degraded intensively and extensively, and shrank to the LLPMin;(4) Neoglaciation during the late Holocene(4000-3000 to 1000 a BP, when permafrost again expanded;(5) Medieval Warming Period(MWP) in the late Holocene(1000-500 a BP) when permafrost was in a relative decline;(6) Little Ice Age(LIA) in the late Holocene(500-100 a BP), when permafrost relatively expanded, and;(7) Recent warming(during the 20 th century), when permafrost continuously degraded and still is degrading. The paleo-climate, geography and paleopermafrost extents and other features were reconstructed for each of these seven periods. | Huijun JIN Xiaoying JIN Ruixia HE Dongliang LUO Xiaoli CHANG Shaoling WANG Sergey S MARCHENKO Sizhong YANG Chaolu YI Shijie LI Stuart A HARRIS | 2019 | Science China Earth Sciences2019，62，8： | 6 |
| 6 | The Variation of Stone Cell Content in 236 Germplasms of Sand Pear(Pyrus pyrifolia)and Identification of Related Candidate Genes显示文摘Stone cells have been described to substantially influence pear fruit quality,as lignin and cellulose are the main components of stone cells.However,there are limited studies on the relationship between the variation and molecular basis of stone cells,lignin and cellulose content among different pear varieties.Here,to reveal the variation of stone cell content within different cultivated species,we collected 236 germplasms of sand pear(Pyrus pyrifolia)at 50 days after flower blooming(DAFB),the key stage of stone cell formation.In our results,we measured the content of stone cells,lignin and cellulose and found that these contents ranged from2.82%to 29.00%,8.84%to 55.30%and 11.52%to 30.55%,respectively.Further analysis showed that the variation coefficient of stone cell,lignin and cellulose content was 39.10%,28.03%and 16.71%,respectively.Additionally,a significant correlation between stone cell,lignin and cellulose content were detected,and the correlation coefficient between the contents of stone cell and lignin(0.912)was higher than between the contents of stone cell and cellulose(0.796).Moreover,the average lignin content(29.73%)was higher than the average cellulose content(18.03%)in stone cells in pear fruits,indicating that lignin is the main component of stone cell in pears.Finally,on the basic of the transcriptome data,we identified 10 transcription factors belonging to bHLH,ERF,MYB,and NAC transcript families,which might be involved in lignin formation in stone cells.qRT-PCR experiments verified coincident trends between expression of candidate genes and stone cell content.This research laid foundation for future studies on genetic variation of stone cells in pear fruits and provided important gene resources for stone cell regulation. | Jiaying Zhang Jiaming Li Cheng Xue Runze Wang Mingyue Zhang Kaijie Qi Jing Fan Hongju Hu Shaoling Zhang Jun Wu | 2021 | Horticultural Plant Journal2021，7，2： | 3 |
| 7 | Self-nanoemulsifying drug delivery system of persimmon leaf extract optimization and bioavailability studies显示文摘 | Li Wanwen Yi Shaoling Wang Zhouhua | 2011 | Int J Pharm2011，420，1： | 1 |
| 8 | Desertification and its relationship with permafrost degradation in Qinghai-Xizang (Tibet) plateau显示文摘 | Meixue Yang Shaoling Wang Tandong Yao Xiaohua Gou Anxin Lu Xuejun Guo | 2004 | Cold Regions Science and Technology2004，，1： | 1 |
| 9 | Desertifica- tion and its relationship with permafrost degradation in Qinghai- Xizang (Tibet) Plateau显示文摘 | Yang Meixue Wang Shaoling Yao Tandong | 2004 | Cold Regions Science and Technol- ogy2004，39，1： | 1 |
| 10 | Cold-region environments along the China-Russia Crude Oil Pipeline and their management显示文摘The cold-region eco-environments along the China-Russia Crude Oil Pipeline (CRCOP) in northern Northeast China are in disequilibrium due to the combined influences of pronounced climate warming and intensive anthropogenic activities.This is evidenced by the sharp areal reduction and northward shifting of the boreal forests,shrinking of wetlands,enhancing of soil erosion,accelerating degradation of permafrost and deteriorating of cold-region eco-environments.The degradation of permafrost plays an important role as an internal drive in the eco-environmental changes.Many components of the cold-region eco-environments,including frozen ground,forests,wetlands and peatlands,forest fires and 'heating island effect' of rapid urbanization,are interdependent,interactive,and integrated in the boreal ecosystems.The construction and long-term operation of the CRCOP system will inevitably disturb the cold-region environments along the pipeline.Therefore,a mandatory and carefully-elaborated environ-mental impact statement is indispensable for the proper mitigation of the ensued adverse impacts.Proper management,effective protection and practical rehabilitation of the damaged cold-region environments are a daunting,costly and long-term commitment.The recommended measures for protection and restoration of permafrost eco-environments along the pipeline route include adequate investigation,assessment and monitoring of permafrost and cold-region environments,compliance of pipeline construction and operation codes for environmental management,proper and timely re-vegetation,returning the cultivated lands to forests and grasslands,and effective mitigation of forest fire hazards. | RuiXia He HuiJun Jin LanZhi L(U) ShaoLing Wang | 2010 | Research in Cold and Arid Regions2010，2，2： | 1 |
| 11 | Cadmium and Its Epigenet- ic Effects 显示文摘 | Wang B Li Y Shaol C | 2012 | Current Medicinal Chemistry2012，19，16： | 1 |
| 12 | The fist report of an Iridovirus like agent infection in farmed turbot, Scophthalmus maximus, in China 显示文摘 | ShiCY Wang YG ShaoL Y | 2004 | Aquaculture2004，236，： | 1 |
| 13 | Permafrost degradation on the Qinghai-Tibet Plateau and its environmental impacts显示文摘 | Wang Shaoling Jin Huijun Li Shuxun | 2000 | Permafrost and Periglacial Processes2000，11，1： | 1 |
| 14 | Desertification and its relationship with permafrost degradation in Qinghai-Xizang(Tibet) Plateau显示文摘 | Yang Meixue Wang Shaoling Yao Tandong | 2004 | Cold Regions Science and Technology2004，39，1： | 1 |
| 15 | Phylogenetic and Expression Analyses of With-No-Lysine Kinase Genes Reveal Novel Gene Family Diversity in Fruit Trees显示文摘With-No-Lysine kinases(WNK) have been reported to be associated with plant growth regulation in Arabidopsis, soybean, and rice, but little is known of their roles in fruits. In this study, a total of 114 WNK genes were identified from 8 fruit trees species, and these WNK genes belonged to 2 classes(I and II) that respectively contain 4(A, B, C, D) and 2 groups(E, F). The WNK genes had variable exon-intron structures and were randomly distributed among most chromosomes of each genus. The expression levels of six of the 18 WNK genes in peach were almost undetectable in fruits, suggesting that they may not be associated with fruit development and ripening. Of the other 12 WNK genes, PpWNK.B1 exhibited stronger stability of expression levels than the best reference genes reported previously in fruits from two peach cultivars. These results suggested that PpWNK.B1 could be a reliable reference gene for gene expression studies of peach fruit. Moreover, qRT-PCR assays yielded evidence that when using single reference gene as internal control, mistakes were more possible, indicating that the use of three reference genes is necessary for gene expression studies. Based on the gene expression profiles validated by qRT-PCR, PpWNK.A1 is predicted to likely be involved in fruit ripening, while PpWNK.A2 and PpWNK.E3.1 are likely associated with early fruit development. The present study represented the WNK genes in fruits, and it will be a valuable resource in continuing investigation of gene regulation network during fruit development and ripening. | Suhao Cao Pingping Hao Weishen Shu Guoming Wang Zhihua Xie Chao Gu Shaoling Zhang | 2019 | Horticultural Plant Journal2019，5，2： | 1 |
| 16 | Geochemical and Nd isotopic variations in sediments of the South China Sea: A response to Cenozoic tectonism in SE Asia 显示文摘 | LiXH WeiGJ ShaoL LiuY LiangXR JianZM SunM Wang P X | 2003 | Earth Planet Sci Lett2003，211，34： | 1 |
| 17 | Changes in per- mafrost environments along the Qinghai-Tibet engineering corri- dor induced by anthropogenic activities and climate warming显示文摘 | Jin Huijun Yu Qihao Wang Shaoling | 2008 | Cold Regions Science and Technology2008，53，3： | 1 |
| 18 | Molecularly imprinted copolymer membranes functionalized by phase inversion imprinting for uracil recognition and permselective binding显示文摘 | WANG Hongying XIA Shaoling SUN Hong | 2004 | J Chromatogr B2004，804，： | 1 |
| 19 | Philadelphia chromosome-positive acute myeloid leukemia with masses and osteolytic lesions: finding of 18F-FDG PET/CT显示文摘 | Zhan Su Fengyu Wu Weiyu Hu Xiaodan Liu Shaoling Wu Xianqi Feng Zhongguang Cui Jie Yang Zhenguang Wang Hongzai Guan Hongguo Zhao Wei Wang Chunting Zhao Jun Peng | 2017 | Frontiers of Medicine2017，11，3： | 1 |
| 20 | Morphogenesis of crgosols and associated soils in the alpine zone of Tienshan, West Chian显示文摘 | Zhao Lin Wang Shaoling | 2002 | Journal of Glaciology and Geocryology(冰川冻土)2002，24，5： | 1 |
您所在的机构暂未开通此部分的功能，请联系管理员