25 August 2004, Volume 26 Issue 4
    

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  • LI Shu-xun, WU Tong-hua
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 377-383. https://doi.org/10.7522/j.issn.1000-0240.2004.0063
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    Some problems relevant to the permafrost temperature regime research were analyzed and discussed in this paper, including the lithology of permafrost, water content, configuration and structure, the relationship between surface temperature and air temperature, the heat flow under ground, the determination of research area and some parameters about the lithology, water content, configuration and structure. Based on the research result of some subjects such as analytical physics, geosciences and climatology, some conclusions were drawn as follows: Firstly, in the case of permafrost temperature regime research, the determination of study area should be based on the time scale of research. Because the influence of temperature and heat flow on permafrost in different depths changes with time, the heat flow of permafrost base should be used as the lower boundary condition to solve the problem of permafrost temperature regime. Secondly, Coefficient N, which reflects the relationship between surface temperature and air temperature, changes annually, seasonally and daily. The duration of ground freezing is essential to get the value of the coefficient. Therefore, it is simple to use the value of air temperature minus surface temperature to describe the relationship between them. Thirdly, on account of the diversity of terrain, surface condition, lithology of stratum and heat flow on the Tibetan Plateau, isotherm cannot be used to map permafrost as a single index, and it is unreasonable to forecast permafrost change in accordance with it.
  • ZHANG Shi-qiang, DING Yong-jian, LU Jian, LIU Shi-yin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 384-388. https://doi.org/10.7522/j.issn.1000-0240.2004.0064
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    Water-heat process in the Tibetan Plateau is significant to global climate change, variance of soil moisture and soil temperature is the key factor of simulating water-heat process. In this paper, a water and energy balance macro-scale hydrological model is used to compare the simulated soil moisture, soil temperature and other fluxes with the observed ones on the step of 1 hour during 399 days in Tuotuohe. The results of soil moist ure are discussed. The changing tendency of the simulated soil moisture in three layers is accordant well with that of observation for more than one year. It is indicated that the Fuchs Equation can properly get the maximum unfrozen water in frozen soil in cold season, and a fairly little accumulated error exists in the simulation. The results reveal that the model is stable in yearly scale and can simulate for a long period in the Tibetan Plateau.
  • LI Zhen, LI Xin-wu, LIU Yong-zhi, REN Xin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 389-396. https://doi.org/10.7522/j.issn.1000-0240.2004.0065
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    In the Tibetan Plateau there are 1 272 709 km2 and 1 146 399 km2 of permafrost and seasonal frozen ground, respectively. The Qinghai-Tibet Railway began to construct in 2002. Permafrost is a disadvantage for engineering construction. There are about 550 km of the railway passing through permafrost regions, including continuous permafrost and some island permafrost. The maximum depth of the active layer at the test site reaches approximately 0.4~1.5 m, the extensive regions of frozen ground hold large amount of moisture in wintertime. The seasonally thawing layer is sensitive to temperature change. It is clear that thawing and temperature rising has a great influence on railway stability. The surface displacement due to seasonally frost heaving and thaw settlement is the main trouble for engineering construction in permafrost regions. One of the maintasks in the operation of the Qinghai-Tibet Highway or the Qinghai-Tibet Railway is to monitor the displacement field of permafrost. The interferometric SAR technique has demonstrated its capability to measure ground deformation in wide range of application. For some applications, especially those involving engineering projects, quantitative application of the InSAR results is required. The seasonal transition of the land surface between frozen and non-frozen conditions affects a number of ecological and hydrological processes. At the same time, the freeze/thaw transition will cause a deformation of ground surface, which is the main factor that should be considered in engineering construction in permafrost regions. In this study, three topics are of special interest. 1) A method developed to map the displacement field by means of InSAR measure with the high accurate DEM; 2) Validation and analysis of the results; and 3) Future work for improving the accuracy of deformation mapping by means of SAR interferometry. Four scenes of SAR SLC images, including Tandem data, are used to produce multiple imterferograms, and 1:100 000 DEM is used to reduce the terrain effect. Using repeated pass differential SAR interferometry, the displacement field is mapped with 0~2.02 cm vertical settlement. The settlement values are validated and compared quantitatively base on precise and accurate geodetic data derived from field measurement, and the environmental characteristics of displacement field are analyzed. The presented results demonstrate that the interferometrical SAR are fairly good for permafrost deformation monitoring, and there is a great potential of SAR data for monitoring the displacement of permafrost caused by frost heaving and thaw settlement for the management of the Qinghai-Tibet Railway. It is believed that short baseline SAR pairs, accurate Delft orbit calculation, further atmosphere correction, and long-time serial SAR data on the study area would help to improve the accuracy significantly.
  • CHE Tao, JIN Rui, LI Xin, WU Li-zong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 397-402. https://doi.org/10.7522/j.issn.1000-0240.2004.0066
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    Along with glacier retreating due to global warming, more and more meltwater cumulates in glacial lakes, resulting in expansion of lake surface. Rapid accumulation of water in glacial lakes, particularly in those lakes adjacent to retreating glaciers, can lead to a sudden outburst of the unstable dams in front of the lakes. The glacial lake outburst flood (GLOF) often has catastrophic effect on downstream regions. The GLOF causes many dangers to local people, as well as to houses, bridges, fields, forests and roads. The lakes at risk are situated in remote and inaccessible areas. Remote sensing provides a feasible method to monitor these glacial lakes. Satellite images (ASTER) acquired in 2000/2001 were interpreted and compared with the report of the First Expedition to Glaciers and Glacier lakes in the Pumqu and Poiqu River Basins, Xizang (Tibet), China. The final results have shown that there are 225 glacial lakes with a total area of 1,062 km2, and there are 24 glacial lakes were identified as the potentially dangerous lakes in the Pumqu basin. It provides the basic information for GLOF mitigation measures, as well as for their monitoring and establishing an early warning system.
  • YAN Shun, MU Gui-jin, KONG Zhao-cheng, NI Jian, YANG Zhen-jing
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 403-410. https://doi.org/10.7522/j.issn.1000-0240.2004.0067
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    Several cross-sections were selected at different elevations, different vegetation zones and different sedimentary faces on the north slopes of the Tianshan Mountains. Substitutive indexes for environmental study (including sedimentary phase, pollen, grain size, magnetic susceptibility, cautery lost, and 14C dating) show that there has been the climatic oscillation of cold/warm and dry/wet since the beginning of the late Holocene, but the arid features did not basically change. There is no significant change in vegetation pattern, including alpine forest, grassland-steppe on low mountain and hill, steppe-desert on the plain. But both of the upper and lower timberlines, developing level of the valley forest, and marshland area on the lowland distinctly change with climatic oscillation. The lakes on plains have significantly varied with environmental change, especially the lake surface area. The periods from 3.1 to 2.4, 1.7 to 1.3, and 1.27 to 0.3 ka BP were high lake level stages. The climate was relatively moist and warm, with high lake level, during the Middle Ages from 1.7 to 0.6 ka BP. The lower timberline of the Tianshan conifer forest moved downward, the forest zone was widened, and the natural environment appeared the optimum time from 1.7 to 1.3 ka BP. Human activity has significantly impacted the environment in latter history period only, and mainly influenced the plain runoff system and the oases. On the plain regions appear river discharge decreasing, shortening of the of the river courses, drying-up of the tail-lakes, northward migrating of the fan-margin, lowering-down of the ground water and spring discharge decreasing. Artificial oases replaced the natural oases. The area of natural oases tremendously decreases, including the lakeshore oases, valley-plain oases, fan-margin oases and delta oases.
  • FENG Hu-yuan, CHENG Guo-dong, AN Li-zhe
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 411-419. https://doi.org/10.7522/j.issn.1000-0240.2004.0068
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    Methane is an important greenhouse gas, which is up to 1.7×10-6m3·m-3 over past 300 years and increasing by a steady rate of 1% per year. Although it has a short residing time (about 8-12 years) in the atmosphere, there are more 20-30 times in absorbing the infrared light and driving the global warming than carbon dioxide. Therefore a considerable and wide interest is focused on the mechanisms of methane production, transfer and oxidation, the relationship between resources and sinks. Methane plays a crucial role in the global methane cycle. There are two resources about methane production: biogenic methane and abiogenic resources. The amount of methane involved in biogenic resources accounts for over 80% in the atmosphere and most is emitted through artificial and natural wetlands. Methanogens are strict anaerobes, which share a complex biochemistry for methane synthesis as part of their energy metabolism and methanotrophs have the unique ability to use methane as sole carbon and energy source. Up to now, scientists have isolated more than 80 species of methane-produced bacteria and over 100 species of methane-oxidized bacteria from a various scale of environments. Many environmental factors such as soil physiochemical properties, climatic factors and vegetation type and human activities affect the emission, transportation, transfer and oxidation by influencing microbial processes directly and indirectly. This may be as a main reason to cause the uncertainty of assessing the emission of methane. It is evident that the study of microorganism diversity and microbial ecology of methane bacteria and microbial-mediated methane cycle will favor regulating and controlling the production and oxidation of methane. More concern should be highlighted in this area. This paper reviewed the microbial-induced methane cycle, isolated diversities of methane bacteria (including methanogens and methanotrophs), various factors affecting the growth and development of methane bacteria and stressed the important of further investigation into the rule of methane emission and oxidation, especially, in natural wetlands under the condition of global change.
  • ZHANG Xin-ping, YAO Tan-dong, TIAN Li-de, LIU Jing-miao
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 420-425. https://doi.org/10.7522/j.issn.1000-0240.2004.0069
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    The humidity effect, namely the markedly positive correlation between stable isotopic ratio in precipitation and dew-point deficit in atmosphere ΔTd, is put forward firstly and the relationship between δ18O in precipitation and ΔTd is analyzed in this paper for the Urumqi and Kunming Stations, which climatic characteristics are completely different. Although the seasonal variations in δ18O and ΔTd have difference for the two stations, their humidity effect is notable. In Kunming Station, the correlation coefficient and its confidence level of the humidity effect are all higher than those of amount effect, showing a marked influence of the psychrometric conditions on stable isotopes in precipitation. Using kinetic model for stable isotopic fractionation and according to seasonal distribution of mean monthly temperature on the 500 hPa at Kunming Station, the variation of δ18O in condensates in cloud at Kunming Station is simulated. A very good agreement between the simulated monthly δ18O and the mean monthly temperature on the 500 hPa is obtained, showing that the oxygen stable isotope in condensates in cloud has temperature effect. Such a result is very different from amount effect of the oxygen stable isotope in precipitation in surface. Based on the simulation for seasonal variation of δ18O in falling raindrops, it can be found that, in the dry season from November to April, the increase, with falling distance, of δ18O in falling drops is remarkable corresponding to great ΔTd, showing a strong evaporation enrichment function for stable isotopes in raindrop as falling; however, in the wet season from May to October, δ18O value in falling raindrops displays an inapparent increase corresponding to small ΔTd, except for that in May. By comparing the simulated mean monthly δ18O in surface with the measured monthly δ18O in precipitation, it can be found that both monthly δ18O series have very good agreement. Averagely, δ18O values are relatively lower because of high moist air, heavy rainfall, small ΔTd and weak evaporation enrichment function of stable isotopes in falling raindrops, under the influence of vapor from oceans; but relatively higher because of dry air, light rainfall, great ΔTd and strong evaporation enrichment function in falling raindrops, under the control of continental air mass. Therefore, δ18O in precipitation at Kunming Station can indicate the psychrometric situation in atmosphere to a certain degree, and thus do the intensity of precipitation and strength of monsoon indirectly. The humidity effect changes not only the degree of stable isotopic ratios in precipitation but also its seasonal distribution due to shifting the strength of evaporation enrichment of stable isotopes in falling raindrops and the direction of net mass transfer of stable isotopes between atmosphere and raindrops. Consequently, it is inferred that humidity effect is probably one of the foremost causations of amount effect.
  • XIAO Jian-zhang, LAI Yuan-ming, ZHANG Xue-fu, YU Wen-bing, ZHANG Shu-juan
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 426-434. https://doi.org/10.7522/j.issn.1000-0240.2004.0070
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    Attracted worldwide attention, the Qinghai-Tibet railway is built on the frozen soil regions more than 550 km long, of which about 100 km are built on high-temperature unstable frozen soil. The key to the success or failure of the railway is whether the embankment under it is stable or not. To resolve the problems of frost heaving and the thawing settlement, to insure the stable of the embankment and the unimpeded move of wild animals, the Qinghai-Tibet railway forms a land bridge on the high-temperature unstable frozen soil. However, up to now, nobody has researched the temperature character of the land bridge in cold regions. In this paper, based on differential equations of the problem on temperature field with phase change, a three-dimensional temperature character analysis of the land bridge built in cold regions with high-elevation was made by using the finite element formulae. The analysis shows that in the coming 20 years, the land bridge built on the regions of high-temperature unstable frozen soil could provide cool energy for the frozen soil greatly and protects the frozen soil under it obviously, and then meets the requirement of thermal stable of the frozen soil under it. Moreover, the analysis also proves that to build land bridge for Qinghai-Tibet railway in high-temperature unstable frozen soil regions is indispensable and feasible.
  • SUN Zhi-zhong, MA Wei, LI Dong-qing
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 435-439. https://doi.org/10.7522/j.issn.1000-0240.2004.0071
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    During 2001-2003, an experimental air convection embankment (ACE) was constructed in Beiluhe Test Field in the Tibetan Plateau. The embankment is built on permafrost foundation with thick ground ice. Both slopes of the embankment were filled in with poorly sorted coarse (5~8 cm and 40~50 cm) crushed rock. It should be called air convection embankment with crushed rock slope protection (ACE-CRSP). The highly permeable ACE-CRSP installation was designed to test the cooling effect of ACE-CRSP concept in a real railway project. Ground temperatures were collected from test sections by sing thermistor sensors. In this paper, based on the ground temperatures taken in the boreholes within the south block-rock and crushed stone slopes, the temperature change was analyzed for different rock diameters and different heat budgets into soil body. The result shows that the mean ground temperature under the block-rock layer is lower than that under the crushed stone layer, and the temperature fluctuating range is larger under the former than that under the latter. It is obvious that the maximum depth of thawing rises under the block-rock layer, which results from the stronger cooling effect of its convection during wintertime. The amount of heat budget displays that for supplying cold energy, the block-rock layer is better than the crushed stone one.
  • CHEN Xiao-fei, DU Yang, MA Wei, ZHANG Yu-long, LI Hong-sheng, XU Xiao-zu
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 440-448. https://doi.org/10.7522/j.issn.1000-0240.2004.0072
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    The characteristic curves of soil freezing and thawing reflect the strength, thermal properties and water and solute transport regularity. In order to study the migration of soil nutrient during soil freezing and thawing, the freezing and thawing curves of umber soil, mixed with solutions of (NH42SO4, KH2PO4 and KCl, respectively, were measured by nuclear magnetic resonance. It was found that the influence of the concentration of KH2PO4 on the freezing and thawing curves is insignificant, but that of KCl and (NH42SO4 are significant, especially that of KCl. Secondary discontinuous point was found on freezing or thawing characteristic curve of some samples mixed with either KCl or (NH42SO4 solutions. Hysteresis widely exists in the freezing and thawing characteristic curves. The temperature range of the obvious hysteresis zone decreases with solute concentration increasing. For the same concentration, the temperature range of the obvious hysteresis zone is the minimum for the samples mixed with KCl solution, followed by that mixed with (NH42SO4, and is the maximum for the samples mixed with KH2PO4.
  • QI Ji-lin, LI Hai-peng, LAI Yuan-ming, ZHU Yuan-lin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 449-453. https://doi.org/10.7522/j.issn.1000-0240.2004.0073
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    In seasonally frozen regions, with the appearance and disappearance of temporary frozen soil layers, the engineering properties of ground may change and consequently is related to stability of constructions in such regions. For this reason, the ground motion in seasonally frozen regions is studied. There are two parts in the study: in-situ measurement and ground motion analysis. Undisturbed soil samples were taken at the same time of in-situ measurement. In this paper the in-situ measurement and analysis of micro-tremor in a site in seasonally frozen area are presented, and the effect on seasonally frozen layers is discussed. Taking the site in Zhangye city in Northwest China as a working site, in-situ measurement of micro-tremor was carried out in 3 orientations, U-D, EW and SN. The measurement was undertaken twice. The first measurement was taken in autumn, when there was no frozen layer at all. In order to analyze the most likely time when the site would be frozen to the maximum depth, climate data were collected from the local meteorological stations. Then the second measurement was taken in winter when the maximum frozen depth maybe appears. The measurement is analyzed and compared with each other. It is found that with the appearance of frozen layer on the top, distinguished period increases; shape of frequency spectrum also changes.
  • ZHANG Xi-fa, XIN De-gang, ZHANG Dong-qing, WANG Xue-rui
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 454-460. https://doi.org/10.7522/j.issn.1000-0240.2004.0074
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    Water migration and variation in subgrade soils is the most active and live factor to the road frost damage in seasonally frozen ground regions. No matter how deep groundwater level is, groundwater may migrate to the upper subgrade at a cutting in freezing period with different extent. Climatic conditions of the road and properties of the subgrade soils all have a strong influence on the vertical migration amount of moisture and the extent of frost heave. It is the vertical migration that causes strong frost heave in the upper subgrade. Other migrations of moisture (including in the slope surface of shoulder, the disabled drain ditch, the crack of pavement, the central isolation strip and so on) may also be the assignable and important factors to lead frost damage to the road. The dryness of the subgrade soils will deteriorate seriously after the road is completed, leading to frost damage.
  • ZHAO Fa-zhang, WANG Jie-jun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 461-465. https://doi.org/10.7522/j.issn.1000-0240.2004.0075
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    An element of vehicle-bridge coupling is established based on train-bridge interaction. A vehicle of train is modeled as an element possessing 4 axles and 10 degrees of freedom. Bridge is modeled as beam elements. Finite element formulas are educed from the equations of motion for whole train-bridge system. The random rail roughness samples are yielded using random numerical method and power spectral density function. Based on present method, a computing program is developed. As an example, the dynamic response and impact factors of a cable-stayed bridge are analysis with various damping parameters and various train speeds.
  • CHEN Ji, CHENG Guo-dong, ZHANG Xi-fa
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 466-473. https://doi.org/10.7522/j.issn.1000-0240.2004.0076
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    Observation of delamination frost heave is of significance in the study of foundation frost damage. There are three main methods of observing delamination frost heave: single frost-heave ruler method, spliced frost-heave ruler method and magnetic-loop method. They are briefly introduced in this paper at first. Then, their advantages and disadvantages are analyzed respectively. The key problems of the single ruler method and their solutions are pointed out. And then, according to the mechanism of frost heave and the law of water migration and ice forming in the freezing soil, comparing surface frost heave and frost-depth brings a new approximate indirect method of observing the delamination frost heave forward. Based on the observation of three proving grounds, located in Yongji and Erlong Irrigation Area of Inner Mongolia and Daqing, the applicability is analyzed from three aspects under different groundwater level and soil property in seasonal frozen area. Simultaneously, the applicability in permafrost is also verified by virtue of data from Jiangcang of Qinghai. Finally, it is pointed out that antitheses can be used only in seasonal frozen area. The method is invalidated in permafrost.
  • AN Li-zhe, DAI Yi-ling, CHEN Tuo, XU Shi-jian, ZHANG Man-xiao, LIU Yan-hong, CHENG Guo-dong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 474-481. https://doi.org/10.7522/j.issn.1000-0240.2004.0077
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    The main anatomical and surface characteristics of leaves of Leontopodium leontopodiodes (Willd.) Beauv. from three habitats of 4 000 m, 3 400 m and 2 500 m a. s. l. in the source area of the Ürümqi River were analyzed and compared by means of light and scanning electron microscope using a new embedding method with PEG and Epon-812. The results indicated that Leontopodium leontopodiodes at the source area of the Urumqi River is the mesophytes with part leaf structural characteristics of xerophytes and hydrophytes. Above the habitat of 4 000 m a. s. l., the surface of cuticle of the leaf epidermis wall of Leontopodium leontopodiodes agrees with granular wax. The other two habitats not agree with granular wax. Many characteristics are distinctly different for different habitats, such as the thickness of leaf, epidermis shape and the pattern of anticlinal wall, and the distribution characteristics of stomatal apparatus, stomatal size, stomatal density, formation of vascular bundle, CTR, chloroplast content of mesophyll tissue and the cuticilar thickness degree of polar "T" shape of guard cells. However, fewer characteristics of the hair-shaped appendant organ and the plane station type of stomata change on the epidermis. It is revealed that the diversity of individual morphology and the combination of characteristics of the leaf morphological structure are correlated with habitats.
  • WU Jian-min, XING Hua, ZHAO Zhi-guang, AN Li-zhe
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 482-487. https://doi.org/10.7522/j.issn.1000-0240.2004.0078
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    Antifreeze proteins (AFPs) are a type of proteins, which exhibit thermal hysteresis activity and inhibit the recrystallization of ice. They were induced under environmental stress and can increase the plant resistance to freezing. AFPs have been found in many freezing-tolerant organisms, including fish, insects, terrestrial arthropods, bacteria, fungi and plants. Until now, several AFPs have been isolated and characterized and five full-length AFP cDNAs have been cloned and characterized in high plants. Among these plant AFPs, the amino acid sequences have shown low homology. In addition, it was found that plant AFPs also could be induced by other factors such as drought, ethylene and abscisic acid besides low temperature. In this review, firstly, the discovery, physiological-biochemical characteristics, tissular and cellular localization, physiological functions, mechanism of interactions with ice crystals, structural model of plant AFPs are discussed; secondly, the application of plant AFPs in agriculture, medicine and food industry is also summarized.
  • MAO Wei-yi, CHEN Chao, DUAN Jian-jun, SU Hong-chao, WANG Su-feng, WANG Jin, GE Fan-yong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 488-495. https://doi.org/10.7522/j.issn.1000-0240.2004.0079
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    The three tributary river systems that contribute flows to the Tarim River (Aksu, Hotan and Yarkant) 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. In 2002, annual virgin flow of about 273.9×108m3 from four mountains basins of Aksu, Hotan, Yarkant and Kaidu-Konque Rivers drain into the Tarim basin, more 46.9×108m3 than average annual streamflow, increasing by 20.7% and more. The Aksu River and Konque-Kaidu Rivers from Tianshan Mountains have a large runoff rising comparing with average annual runoff, and keep normal runoff in Yarkant River from the Karakorum and Hotan River from the West Kunlun Mountains. The annual virgin flow of Aksu River in 2002 had 109.8×108m3,more 28.4×108m3 than average annual streamflow, increasing by 34.8%; and 57.10×108m3 for Kaidu-Konque River,more 22.24×108m3 than average annual streamflow, increasing by 63.8%; 61.92×108m3 for Yarkant River,less 5.28×108m3 than average annual streamflow, decreasing by 8.0%; 45.03×108m3 for Hotan River,same as average annual streamflow. Most of this water is consumptively used before reaching the confluence, total consumptive water of four source streams sum up 219.1×108m3, occupy up 80% of annual virgin flow from mountains basin. The total annual runoff of 56.48×108m3 drain into the mainstream of the Tarim River from the four source streams in 2002, occupy up 20% of annual virgin flow from mountains basin. The interzone consumed water of the Tarim River mainstream are estimated to be 25.42×108m3 for the upper course, account for 46.2% of annual streamflow of Aler Station, the largest consumed interzone of the Tarim River mainstream; 24.55×108m3 for the middle course, 44.6% of Aler ones and 7.38×108m3 for the downstream course, 13.4% of the Aler ones. The consumed water of both upper and middle streams course sum up 49.97×108m3, account for 90.8% of annual streamflow of Aler Hydrological Station.During July 20 to November 10,2002, total 114 days, the fourth ecological emergency water diversion project was carried out in the lower reaches of Tarim River, transfer water from Bosten Lake to the Taitema Lake. Outflow 3.313×108m3 drains into 300 km upstream of Taitema Lake, from Daxihaizi Reservoir, and a 28.74 km2 water area appeared in Taitema Lake in 2002.
  • WANG Shun-de, LI Hong-de, HU Lin-jin, SU Hong-chao, CAO Xiao-li, SUN Ben-guo, LI Chun-mei, MAI We-iyi, WANG Jin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 496-502. https://doi.org/10.7522/j.issn.1000-0240.2004.0080
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    The Tarim River Basin is surrounded by mountains on three sides and is a closed-basin with no outlet to the sea. From the confluence of its three main contributing tributaries, the Tarim River mainstream extends 1321 km to Taitema Lake. The three tributary river systems that contribute flows to the Tarim River (Aksu, Hotan and Yarkant) 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. There are numerous other rivers coming down from the mountains that disappear into the desert. A number of rivers fed by snowmelt and glacier melt begin in the mountains and drain into the basin. In 2002, annual virgin flow of about 273.9 108m3 from four mountains basins of Aksu, Hotan, Yarkant and Kaidu-Konque Rivers drain into the Tarim basin, more 46.9 108m3 than average annual streamflow, excessive more 20.7%. The Aksu River and Konque-Kaidu Rivers from Tianshan Mountains have a large runoff rising comparing with average annual runoff, and keep normal runoff in Yarkant River from the Karakorum and Hotan River from the West Kunlun Mountains. Most of this water is consumptively used before reaching the confluence, total consumptive water of four source streams sum up 219.1 108m3, occupy up 80% of annual virgin flow from mountains basin. Actual annual consumptive water were measured to be 65.90 108m3for Aksu, 60% of annual virgin flow; 61.92 108m3for Yarkant,no water drain into the mainstream of Tarim River; 36.45×108m3 for Hotan, 80.9% of annual virgin flow; 54.76×108m3 for the Kaidui-Kongque, 95.9% of annual virgin flow.
  • SI Jian-hua, FENG Qi, ZHANG Xiao-you
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 503-508. https://doi.org/10.7522/j.issn.1000-0240.2004.0081
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    The heat-pulse technique was applied to study the stem sap flow of Populus euphratica in April and May of 2003. The results show that, in the natural conditions, the intensity of sap flow of Populus euphratica was 0.13~0.15 L·cm-2·d-1.The diurnal change of volume of sap flow showed a minor fluctuations.The velocity of sap flow of Populus euphratica at different depths below the cambium showed the same temporal change. At 12:00 it reached the maximum, and so did its difference . At night, the ascent of sap flow could be observed in the above main tree species owning to the existence of root pressure.The difference of sap flow rate at different direction could also be observedin stem section of P. euphratica. A comparison of thesap flux density of P. euphratica is made with that of Populus deltoids Bartr.cv.‘Lux’ex. -69/55, Pinus tabulae formis, Betula dahurica, Acer mono, Populus popular etc.
  • WU Jin-kui, DING Yong-jian, WANG Gen-xu, SHEN Yong-ping
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2004, 26(4): 509-516. https://doi.org/10.7522/j.issn.1000-0240.2004.0082
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    Study of the water sciences in the cold and arid regions using traditional methods, because of the particularity in geography and complexity in geological environment, faces more difficulty, such as large area, hard working condition and poor previous research. Isotopic techniques, which have been used in water sciences since the 1950s in the world, were firstly used in China in the end of the 1970s. As a kind of new method, they have been widely used in cold and arid regions since the 1980s. In the last 20 years, many advances have been achieved in study of cold and arid regions in China. They mainly include: 1) stable isotopes studies in precipitation, especially in cold regions such as the Tibetan Plateau; 2) some new understanding of original of ground water in arid regions; 3) new isotopes, such as chlorine, boron and lithium, are used in the research of salt lakes; 4) many isotopic sections such as ice cores in cold regions and water bodies in arid regions have been established and many useful ancient geological and environmental information have been picked up from those sections; 5) isotopic fractionation theories in evaporation are studied and advanced. Along with the development of science and technology and with the improvement of isotope measurement levels, isotopic techniques will be used in a wider field in water sciences in cold and arid regions and will be achieved more advance.