25 August 2007, Volume 29 Issue 4
    

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  • YAO Tan-dong, PU Jian-chen, TIAN Li-de, YANG Wei, DUAN Ke-qin, YE Qing-hua, Lonnie G. Thompson
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 503-508. https://doi.org/10.7522/j.issn.1000-0240.2007.0073
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    The Naimona′nyi Glacier,which is located on the southwestern Tibetan Plateau,has experienced rapid retreat in the past 30 years and showed an accelerating recession in the recent years,according to the glaciological field survey from 2004 to 2006.Several branches of the Naimona′nyi Glacier separated from the main body,which means obvious retreat.The mean retreat rate was 5.5 m·a-1 in the past 30 years and 7.7 m·a-1 from 2004 to 2006,which indicates an accelerating glacier recession recently.The mean annual mass balance was -658 mm w.e.q.and the surface elevation decreased 1.35 m at 6 050 m a.s.l and 2.85 m at 4 800 m a.s.l due to strong surface ablation from 2004 to 2006.Moreover,meteorological station record of Burang indicates that the annual mean temperature has a dramatic increase since 1999,while annual precipitation has obviously decreased in the past 33 years.In a warming and arid climatic situation,mass deficits are inevitability.More rapid glacial retreat would be expected if the climate warming and arid condition continue.This will seriously affect water resources and lead to serious social consequences.More attention should be paid to the behavior of the Himalayan glaciers.
  • CHEN Xiao-qing, CUI Peng, YANG Zhong, QI Yong-qing
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 509-516. https://doi.org/10.7522/j.issn.1000-0240.2007.0074
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    There are many glacial lakes in the Poiqu River basin,Nyalam County,Tibet Autonomous Region.Based on interpreting the remote sensing data of Landsat satellite,2000/2001,the distribution and area of glacial lakes are obtained.Compared with the data of 1987,it is found that their number and area changed greatly: the area of glacial lakes increased 46% and the number of the lakes in area over 0.02 km2 increased 11%.Especially,the Galongco and Gangxico increased 104% and 118%,respectively.Field investigation revealed the overfall conditions of some key lakes,the stability of moraine dams,and the impact of glaciers.Using direct distinguishing and risk indexes of glacial lake outburst(Idl),respectively,two types of risk assessments have been completed.Risk assessment shows that there are nine glacial lakes at high dangerous degree,three at middle degree,and two at stable state and the other 35 at relative stable state.In this basin,there are high danger regions in the lower reaches of Chongdui gully,Keya gully and the confluence spot of Keya gully and Poiqu River,and of middle degree,the lower reaches of Tajiling gully, Rujia gully and Zhangzang gully,and safe regions in the other places.In order to mitigate harm to Nyalam and Zham port,a series of countermeasures is put forward,such as: 1) designing mitigation programme on the base of risk assessment,2) pre-warning and emergency programme,3) periodical professional measure and 4) public warning and prevention system.
  • GUO Liu-ping, YE Qing-hua, YAO Tan-dong, CHEN Feng, CHENG Wei-ming
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 517-524. https://doi.org/10.7522/j.issn.1000-0240.2007.0075
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    Based on remote sensing(RS) and geographical information systems(GIS) techniques,using 4 periods of data,including 1:50000 topographic maps that were published in 1974,digital images from Landsat TM in 1990,Landsat ETM+ in 1999,ASTER in 2003 and Digital Elevation Model(DEM),in this paper the glacial landforms in Mapam Yumco Basin in Tibetan Plateau are mapped,and the glacial landform area,variations of glacierized area and lakes in the past 30 years are studied.It is found that the glaciers in Mapam Yumco Basin have been retreating since 1974.In the recent years,glacier retreat is accelerated.It also shows that glacier melt rate on the sunny side is faster than those in the shadow slope,and smaller glaciers in steeper slopes melt faster than those in flat terrain.From 1974 to 2003,glacier wastage was about 7.27 km2,or 6.77% of the total area,with an average retreat rate of 0.24 km2·a-1.Lake area was obviously in reduction in the last 30 years,shrinking from 1974 to 1999,but expanding from 1999 to 2003 to some extent.Many small lakes have disappeared.Lake shrinkage was smaller and smaller and then has shifted to lake expansion since 1999.But generally speaking,lake area was in shrinkage from 1974 to 2003,with a total area decrease of 37.58 km2,accounting for 4.81% of the total area,and an average retreat rate of 1.25 km2·a-1.In addition,the glacier and lake variations with meteorological data during the last 30 years in the basin were analyzed.According to meteorological data from the Burang Station(with an elevation of 3 900 m a.s.l.),which is located in the southwest of Mapam Yumco basin,the average air temperature increases very obviously.Temperature increase in the Mapam Yumco basin consists with a prevailing warming over the Tibetan Plateau during the last decades.Annual precipitation and annual evaporation decreased slightly as shown in its linear fitting.The glacier retreat was most likely due to the negative glacial mass balance and was affected by rising temperature and decreasing precipitation over the Tibetan Plateau.Early lake decrease was likely to be caused by less precipitation in the basin.On the other hand,lake expansion has accelerated since 1999,which was most likely due to more water supplies from intensive melting of glaciers,in addition to less water loss due to evaporation and less precipitation income in the basin.
  • FU Yang, LI Feng-xia, ZHANG Guo-sheng, YANG qiong, ZENG Xiao-qing
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 525-535. https://doi.org/10.7522/j.issn.1000-0240.2007.0076
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    The Three River Sources areas and the regions around Qinghai Lake are the two important ecosystems in Qinghai Province.Based on the typical vegetation monitoring data and surface meteorological data from 1987 to 2004,combining with the remote sensing data of satellite NOAA/AVHRR and investigated data,the main degenerative characteristics of natural grasslands are analyzed.The main characteristics are: degenerative pasturelands area with moderate severity increasing with a speed of 200,000 square kilometers per annum in average;the area with productivity less than 750 kilogram per square kilometer accounting for 26.99% of the total area of the province.Output and height of grass in the Three River Sources areas decrease with the tendencies of 4.48 to 16.48 kilogram per annum and 0.16 to 0.80 centimeter per annum.The linear descending rate of dominant plant numbers are 11 and 16 plants per annum,respectively. The growth percentage of Cyperaceae kind’s pasture in anthesis and seed autumn period decreases 25% to 50%.Pasture output and height in the regions around Qinghai Lake decrease with a speed of 3.05 to 4.64 kilogram per annum and 0.75 to 1.28 centimeter per annum;the proportion of Poaceae as an eminent representative kind decreases 1% to 3%.The descending rate of temperate steppe and temperate desert,which lie in south of the Qinghai Lake,are 0.25% and 0.38% per annum,respectively.According to the above mentioned,the degeneration of pasture in Qinghai Province might attribute mainly to environmental controlling mechanisms of nature and human activity.In this paper,the grassland degenerative mechanism and eco-process degeneration are analyzed.On one hand,among all the natural controlling factors,the tendency of drying and warming is the first important factor for the degeneration.It affects the growing season,pasture output and the community structure of pasture.Besides,pasture degeneration is aggravated owing to the increase of various extreme weather phenomena and climatic disasters since the 1990s;on the other hand,human controlling factors,such as overloading of livestock,population increasing and uneven grazing,further aggravate eco-functional degeneration of nature pastureland.
  • YANG Jin-hu, SHEN Yong-ping, WANG Peng-xiang, YANG Qi-guo
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 536-542. https://doi.org/10.7522/j.issn.1000-0240.2007.0077
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    Using the daily minimum temperature data of 100 stations in Northwest China in 1960-2004,the thresholds of daily extreme low temperature are determined for different stations,diagnosis of the frequencies of temporal and spatial distributions of annual extreme low temperature events is made for the recent 45 a,and their response to regional warming in Northwest China is analyzed.The result shows that consistent anomaly distribution is the principal spatial mode of the frequencies of annual extreme low temperature events in Northwest China;it is found that the spatial mode can be divided into five key areas: north of Xinjiang Region,north of Qinghai Province,east of Northwest China,south of Xinjiang Region,and the plateau in south of Qinghai Province; It is proved that the frequencies of extreme low temperature events show a remarkable decreasing tendency in the north of Xinjiang Region,north of Qinghai Province,east of Northwest China and south of Xinjiang Region,with some abrupt changes.However,there is a weak decreasing tendency in the plateau in south of Qinghai Province.It is also found that the vibration periods of 13~15 a and 7-8 a are displayed very clear in all the five key areas.It is also proved that the frequencies of extreme low temperature events in Northwest China show a remarkable negative response to regional warming.
  • Arkin Turak, Askar Mamat, Tursun Rusul, WANG Xiao-feng, SHEN Yong-ping, MAO Wei-yi, WANG Shun-de
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 543-552. https://doi.org/10.7522/j.issn.1000-0240.2007.0078
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    The Tarim Basin is in northwestern China,in the southern part of the Xinjiang Uygur Autonomous Region,and the total area is 5.5×105km2.High mountains around the basin prevent ocean air from flowing into the basin.High temperatures,strong winds,and high evaporation rates in the basin result in a very dry climate;annual precipitation averages about 30-60 mm.Surface water and groundwater,recharged mainly by the melting ice and snow from the mountains around the basin,nourish various oases in the basin.Total water resource is 429×108m3 in Tarim River basin,with relatively scarce water and very weak ecological environment.Glaciers cover about 23628.98 km2 of the mountains around the Tarim River Basin,with 2669.435 km3 ice volume;the melt water resources released from the glaciers is about 15×109m3 per year, roughly 40% of wholly surface water in the Tarim Basin.A number of rivers fed by snowmelt and glacier melt begin in the mountains and drain into the basin with average annual virgin flow of about 35 billion m3.Peak flow months in the rivers are July,August and September.Lowest flow occurs in the period from January through April.Around the rivers may be found oases of small villages and agriculture.The Aksu,Hotan,Yarkant and Kaidu-Konque Rivers are four source rivers of Tarim River drainage.The three tributary river systems that contribute flows to the Tarim River(Aksu,Hotan and Yarkand) join just above the Aler gauging station where the Tarim River begins.In addition the Kaidu-Konque River Basin,which is hydrologically separate from the Tarim River,contributes water to the Tarim River by means of a man-made transfer channel.A number of other subbasins exist within the Tarim Basin that do not contribute flows to the Tarim River because all of their flows either naturally evaporate in the desert or are used in irrigated agriculture areas.The two main subbasins in this category are the Kashgar River and the Weigan River.The Tarim River had historically nine river water systems with 144 tributaries combined as a Tarim River System.As climate changing and human activities are increasing to affect on the ecological environment,the Tarim River now become a pattern of four sources river systems and a mainstream system.Based on hydro-meteorological monitoring data including precipitation,evaporation,runoff,floods,bedload,and water quality in Tarim river basin in past 50 years,this paper details with the deterioration of the ecological environment causes and recent changes of the river hydrological characteristics in the Tarim River Basin.
  • MAO Wei-yi, Yusup Abudula, CHENG Peng, DONG Ke-peng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 553-558. https://doi.org/10.7522/j.issn.1000-0240.2007.0079
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    The Super-flood and its cause of the rivers on the northern slopes of the Middle Kunlun Mountains in 1999 is analyzed,using the daily runoff and precipitation of hydrological stations,the 0 ℃ level and 500 hPa temperature of Hotan meteorological observation,and the height field of NCEP/NCAR.The flood peak in 1999 is the maximum in the instrumental records. It was a medley flood caused of snow-ice melting water and heavy rain.The precipitation from spring to early summer was more then the average.The 0 ℃ level and 500 hPa temperature were lower than the average.Snow cover was deeper.The 0 ℃ level and 500 hPa temperature increased rapidly from the end of July to the early August,and then lasted a few days.The ice and snow were melting rapidly.At the same time,a heavy rain occurred in the mountains.The circulation system causing the flood was characterized by a high press located upon the Qaidam basin of the northeast Tibetan Plateau and a trough of Central Asia moved eastward to the northern piedmont of the Middle Kunlun Mountains.
  • XIE Fu-ming, MAO Wei-yi, ZHANG Jian-gang, GAO Qian-zhao, SHEN Yong-ping, WANG Jin, WANG Shun-de
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 559-569. https://doi.org/10.7522/j.issn.1000-0240.2007.0080
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    In 2005,annual virgin flow of 272.1×108m3 from four mountains basins of Aksu,Hotan,Yarkant and Kaidu-Konque Rivers drain into the Tarim Basin,more 47.2×108m3 than average annual streamflow of 224.9×108m3,increasing by 21%,is an abundant hydrological year.The total annual runoff from the four source rivers in 2005 ranked by No.5 in last 49 years series of 1957-2005.The runoffs in Aksu,Hotan,and Yarkant Rivers in 2005 are a wet year,increasing range of 22%~25% by compared to the mean annual runoff,and the Kaidu-Konque River is a normal year in 2005.The annual total virgin flow of Aksu,Hotan and Yarkant Rivers above the Aler gauging station are 236.3×108m3 from the mountains basins,and of the Kaidu-Konque River from Tianshan Mountains 35.81×108m3.The total discharge of the four source rivers into Tarim River is 56.88×108m3 in 2005,which three tributary river systems(Aksu,Hotan and Yarkant) contributes 53.97×108m3 flows to the Tarim River.Most of this water is consumptively used before reaching the confluence,total consumptive water of four source streams sum up 216.6×108m3,occupy up 79.6 %of annual virgin flow from mountains basin.The proportion of consumed water of upper,middle and downstream occupy the whole consumed water of Tarim River mainstream comparing with their own woodland proportion respectively,the proportion of consumed water was more in the upper stream course,was a little in the middle streams course,and was correspond in the lower course.Water quantity has been drastically reduced and water quality has deteriorated dramatically in the lower reaches of the Tarim River which have negatively impacted irrigated agriculture and pasture lands.Based on the comprehensive governance project of the Tarim River at present,we still need a long-term comprehensive plan for the Tarim river basin to the ecosystem building as a fundamental engineering,by the macro-regulation of water resources management,economic and technological means, and to ensure sustainable water resources development and utilization of the Tarim River.
  • YAO Yu-bi, YIN Dong, WANG Rong-yuan, DENG Zhen-yong, ZHANG Xiu-yun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 570-577. https://doi.org/10.7522/j.issn.1000-0240.2007.0081
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    Using the main meteorological and ecological data observed in the grasslands of the first meander of the Yellow River,the climate changes and eco-environment effects of the grasslands in the first meander of the Yellow River were analyzed.The results show that in the first meander of the Yellow River,the annual precipitation tended to decrease and fluctuated with three periods: 2~4 years,6~7 years and 10~11 years.The annual mean temperature was remarkably warmer than that in other regions of China;the departure of annual temperature was low before 1983 and high after 1984.The annual mean aridity index of the grasslands tended to increase.There are many serious ecological problems in this area at the present time: fearful degeneration of ecological,desertification of grassland,obvious shortage of water resources,and quick decrease of bio-diversity.All of these are caused by both climate changes and human activity.
  • ZHAO Yi-zhou, MA Yao-ming, MA Wei-qiang, LI Mao-shan, SUN Fang-lin, WANG Lei, XIANG Ming
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 578-583. https://doi.org/10.7522/j.issn.1000-0240.2007.0082
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    Based on the soil temperature and soil moisture data obtained in GAME/Tibet(1996-2000) and CAMP/Tibet(2001-2010),Variation features of soil temperature and soil moisture in different depths on different sites are analyzed.It is found that the variation of daily mean ground temperature above 10 cm has a one-year period.The variation can be showed as a sine curve.The yearly maximum temperature is in July and August.The phase of soil temperature variation in deeper layer is lagged behind that of the shallower layer. The cooling of the soil is quite slow.However,the warming of the soil is fast in spring and summer.Such phenomena may be associated with the feedback processes of snow cover,albedo,long wave radiation and the heat of condensation.The change of yearly climate can be reflected in the depth of 40 cm at least.The variations of daily mean soil moisture in different depths have no pronounced change.The variations of monthly mean soil moisture in different depths change distinctly.Soil moisture is dependent on summer precipitation.
  • WANG Chang-ke, LU Xian-guo, CAI Zu-cong, LUO Yong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 584-588. https://doi.org/10.7522/j.issn.1000-0240.2007.0083
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    The meadow soil in the Zoigê Plateau could consume atmospheric CH4 at a rate of-0.092~0.125 ng·g-1·h-1,and the potential CH4 oxidation rates decreases with increasing soil depth.The peat soil CH4 releases to atmosphere at a rate of 0.236~1.088 ng·g-1·h-1.Both soils can oxidize high-concentration CH4(9000 μL·L-1),but the peat soil can oxidize high-concentration CH4 more quick than the meadow soil does.Different soil layers have almost the same potential of oxidizing high-concentration CH4.CH4 emission form the peat land decreases with the increase of soil CH4 oxidation as the water level dropping in the peat land.
  • JIANG You-yan, REN Jia-wen, QIN Xiang, XIE Ai-hong, WANG Ye-tang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 589-594. https://doi.org/10.7522/j.issn.1000-0240.2007.0084
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    Diurnal mean variation and variations of mean daily variations of global radiation,surface short-wave radiation,surface longwave radiation,atmospheric counter-radiation are analyzed by using the radiation parameters obtained from the automatic weather station over the Ruopula pass of the East Rongbuk Glacier(at an elevation of 6523 m) from May 1 to July 22,2005,the surface albedo and the radiation balance.The short-wave radiation has a big change with the solar elevation angle increasing,and the daily global radiation has a good correlation with the surface short-wave radiation.The surface albedo is higher due to new snow always falling.Diurnal variation of atmospheric counter radiation lags for 2 hours behind the surface long wave radiation change,with a daily variation larger than that of the surface long-wave radiation.Diurnal mean net radiation changes with solar elevation angle increasing.There is an increasing tendency of the daily radiation balance during the observing duration.
  • QU Wei, NIU Shu-wen
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 595-602. https://doi.org/10.7522/j.issn.1000-0240.2007.0085
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    Water is invaluable,irreplaceable natural resources.It is also the basic condition of the life,surviving and production in oases.In order to maintain the oasis’ stabilization and to realize the sustainable development,it is necessary to strengthen the protecting,rationally developing and utilizing the available water resources.According to the characteristics of the physical geography conditions and the formation of water resources,and their distribution and transformation in the arid inland river basins,a basin can be divided into two parts: runoff formation part and runoff dissipation part. In the former,which is distributed over the mountainous area,more than 90% runoff is form.Of the runoff formation part the white "Solid Reservoir" from the high-mountain glacier-snow and the green "Plant Reservoir" from the mid-mountain forest belt should be protected earnestly,owing to their important function for stabilizing and adjusting the water sources;The latter,which is located in the plain areas before mountains,is centralized in artificial and natural oases,the regions of strongly developing and utilizing water resources and human activity.So in this part,it is very important to control the water consumption,water pollution and to exploit rationally the groundwater in order to protect the water resources.The correlative departments and institutes should research and establish a mechanism of ecological compensation as soon as possible,definitude the benefit relationship among the Water Right,Existent Right and Development Right in order to grant the ecologically vulnerable areas more surviving and developing chances and spaces,and to constitute the strict laws and statutes about the regional water resources protection to avoid the tragedy of developing economy in the ecologically vulnerable areas depending on destroying the eco-environment.
  • XU Liu-bing, ZHOU Shang-zhe
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 603-612. https://doi.org/10.7522/j.issn.1000-0240.2007.0086
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    Tectonic uplift and climate change are two key factors controlling the river terrace formation in hinterlands.Rivers in different areas,however,respond to the two drivers in different ways.There are six river terraces on both sides of the Yajin Section of Shuo Qu,which are located in the tectonically active area in western Sichuan Province and are climatically controlled by the south Asian monsoon.Electron spin resonance(ESR) and thermoluminescence(TL) techniques were used to date the sediments from the five higher terraces(T2~T6) and the glacial sediments adjacent to the terraces.The evolution processes of the five terraces are analyzed on the basis of the dating results and the geomorphological and sedimentological characteristics of the terraces.It is revealed that the straths of the terraces (T2~T6) formed during the glacial-interglacial transitions.The sediments on the straths deposited during glacial periods.The incisions for forming these terraces began at the late glacial period,corresponding to the late periods of marine isotope stages 2,6,8,14,and 16,respectively.The incision ratio of the Yajin Section of the Shuo Qu was ~1.22 mm·a-1 since the late marine isotope stage 16,less than the uplifting ratio of 2 mm·a-1 in this region,which is consistent with the previous conclusions that incision ratio was no more than uplifting ratio.
  • JU Yuan-jiang, LIU Geng-nian, WEI Xia
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 613-616. https://doi.org/10.7522/j.issn.1000-0240.2007.0087
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    The theory that equilibrium line altitude acts as a proxy of climate changes is discussed.Based on the abundant observation data on the Glacier No.1 at the headwaters of Ürümqi River in Tianshan Mountains, since the 1960s,a statistical equation relating the present equilibrium line altitude and climate is established and improved,which is verified of rationality in the region.Extrapolating the equation to the second phase of the Little Ice Age of the glacier,and inferring the equilibrium line altitude at that time from maximum elevation of lateral moraines,the climate condition during the phase can be determined.The result is closed to the previous outcomes deduced by other methods.All these show that taking the equilibrium line altitude of alpine glacier as a proxy of climate changes and calculating the climate condition from the equation is feasible.
  • XU Qi-yun, GUO Hui, YIN Xian-zhi, XU Wen-jun, SHi Zhi-juan, HUANG Tao, XI Li-zong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 617-625. https://doi.org/10.7522/j.issn.1000-0240.2007.0088
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    Based on the study results of water resources,climate and glacier variations in the Shiyang River Basin and its adjacent regions,the features of dryness/wetness evolution since 10 ka BP are investigated and its variation series is built.There are seven wet and six dry climatic phases recognized.Furthermore,there are four features in the main climate change in the last 50 a.It is found that the mean annual precipitation in the oasis in the region from 1971 to 2000 was higher than that from 1951 to 1980,but the temperature change in the oasis was not evidence.Meanwhile,the precipitation in the edge of the high mountains and the desert decreased evidently,with an increasing temperature.Furthermore,the mean annual evaporation in most of the region had decreased 10~131 mm,the days of the mean annual sand storm and the thunderstorm had decreased too.
  • WANG Xin, LIU Shi-yin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 626-635. https://doi.org/10.7522/j.issn.1000-0240.2007.0089
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    Due to climate warming in the recent decades,moraine-dammed lake outburst hazards are increasingly threatening people and property.Great progress has been made on the researches on the moraine-dammed lake outburst hazards,because they become a wide and intensive focus.The researches on moraine-dammed lake hazards experienced the processes from field survey for typical moraine-dammed lakes to remote sensing combined with field survey in large-scale regions,from qualitative,semi-quantitative calculation to quantitative computation,from empirical formula based evaluation to simulation based on physical mechanisms.This paper begins with the identification and variation detection,and summarizes the current studies of the causes and mechanisms of moraine-dammed lake outburst;the assessment index systems involved the morainedammed lake outburst risks,the possible simulation ways for moraine-dammed lake outburst floods and debris flows,and their mitigation measures.In the end,the paper outlines the prospects of the researches on moraine-dammed lake outburst hazards,i.e.,1) using remote sensing combined with field survey so as to make the assessment from qualitative to quantitative,2) using multi-measures with multi-data sources in order to simulate the moraine-dammed lake outburst hazards systematically,3) using mitigation techniques integrated with humanity environment factors to remedy the outburst hazards.
  • CHANG Xiao-xiao, MA Wei, WANG Da-yan
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 636-639. https://doi.org/10.7522/j.issn.1000-0240.2007.0090
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    A large test program was conducted on the deep clay in East China to investigate the mechanic behaviour in the process of axial compression and triaxial compression.At the same time,the effect of negative temperature and confining pressure on the strength of frozen clay was analyzed.It is found that the stress-strain curves at high confining pressure belong to the strain hardening type and the strength of frozen clay responds intimately to the confining pressure in the range of the tested confined stress.With respect to temperature,the strength increases with temperature decreasing.
  • LI Dong-wei, WANG Ren-he, HU Pu, CUI Hao
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 640-644. https://doi.org/10.7522/j.issn.1000-0240.2007.0091
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    Based viscoelastic-plastic model of frozen soil,using the method in which the temperature field and the large deformation field are coupled,a plane FEM program which can simulate the frozen soil in cold regions is proposed.The viscoelastic-plastic constitutive model for geo-materials is embedded into the commercial FEM software ADINA as a user’s subroutine.The FEM numerical simulation result of the cone-shaped pile model is close to the model test result,with a similar regularity.This result verifies that viscoelastic-plastic constitutive model of couping temperature freedom-degree is correct and reliable,which can be taken as a reference for designing cone-shaped pile in frozen soil.
  • HAO Jia-qian, JI Yan-jun, HE Nai-wu, WEI Zhi, YANG Si-zhong, HE Rui-xia, JIN Hui-jun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 645-652. https://doi.org/10.7522/j.issn.1000-0240.2007.0092
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    Under a warming climate and resultant accelerated degrading permafrost,warm permafrost might occur in a large extent.The technical and economic feasibility and environmental protection for the design principle of permafrost protection will be significantly challenged.The prethawing technique of permafrost,if applied properly to engineering infrastructures and foundation and geotechnical settings in warm permafrost regions,might ensure the technical feasibility and long-term stability of engineering foundations.The prethawing techniques of permafrost foundations are reviewed and prospected,which include the basic steps and concerned solutions during the design,construct and operation/maintenance phases,based on the studies and experiences on cold regions engineering and the successful application cases of prethawing techniques in China and overseas.The three basic steps are: 1) thawing permafrost before construction,2) consolidation and compaction of thawed soil,and 3) keeping the thawed,frost-susceptible soils from being refrozen and frost heaving. Commonly prethawing techniques used for permafrost include,but not limited to,1) convective warming with hot steam,hot or cold water,2) electric heating,and enhanced warming by modifying ground surface.The techniques for keeping the thawed soils from being refrozen mainly includes modification of ground surface,such as reduction of surface albedo,and/or alteration of soil structures to have a function of thermal insulation or diode,and application of active and passive warming devices or systems,like thermosyphons.Some cases of prethawing techniques in Northeast China,such as the Mohe Airport,were reviewed.
  • LI Qing-xu, LIU Guang-xiu, SHAO Lin-hui
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 653-658. https://doi.org/10.7522/j.issn.1000-0240.2007.0093
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    By introducing the basic elements,approach and count measure of the hierarchy analysis,using this analysis method to study the assessment of ecological-environmental impact of speedway,taking the Baoji-Tianshui Speedway as an example,the selection of the alternative schemes in assessment of ecological-environmental impact of speedway is analyzed.The result shows that this analysis method is not only an effectual method in solving the problem of selection of the alternative schemes in the assessment of ecological-environmental impact of speedway construction,but also improves notably the rationality,and it has a better consistency with the truth.At last,the advantage and disadvantage of this method in the assessment of ecological-environmental impact of speedway is discussed and a suggestion is provided in the study of the assessment of ecological-environmental impact of speedway for the future research.
  • XU Man, ZHANG Ai-jun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 659-663. https://doi.org/10.7522/j.issn.1000-0240.2007.0094
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    Using gray theory,the scientometrical indexes based on the articles abstracted from Science Citation Index Expanded(SCI-E) database on the arid land research by Chinese authors were analyzed and a gray model was built to predict the status and tendency of arid land research in China.Results show that the various scientometrical indexes have increased obviously over the last eleven years and will keep the strong growing tendency in the following years(2006-2008).A series of core supporting disciplines with comparatively firm structure has formed,of which the article yield is not stable yet.Their academic away,measured by article citation indexes,is a little lower than that of international companions,and is much higher than that of the other fields of domestic sciences.
  • JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 664-667. https://doi.org/10.7522/j.issn.1000-0240.2007.0095
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  • JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2007, 29(4): 668-670. https://doi.org/10.7522/j.issn.1000-0240.2007.0096
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