25 June 2005, Volume 27 Issue 3
    

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  • LI Ying-nian, GUAN Ding-guo, ZHAO Liang, GU Song, ZHAO Xin-quan
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 311-319. https://doi.org/10.7522/j.issn.1000-0240.2005.0048
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    Annual mean soil temperature at 0 to 160-cm depths is higher than 1~8℃ and annual mean air temperature is about -1.7℃ in Haibei alpine meadow. Mat-Cryic cambisols under vegetation belongs to seasonal frozen soil. Because of low air temperature, it is possible that frozen soil may form in all seasons. A stable layer of frozen soil can form from November. The frozen soil layer reaches the deepest, about 230 cm, in the period from March to April. Surface ground of the frozen soil thaws from March to April. The process of thawing also begins from the bottom of the frozen soil layer, with a lightly thawing rate. Process of thawing can last to the last ten days of June, or the first ten days of July. The seasonal frozen soil plays an active role on vegetation production in the alpine meadow. The role is: 1) The seasonal frozen soil supplies an ample water resource, which compensates the precipitation not enough in the period from end of the spring to initial of the summer, for plant growth, especially, for initial nutrient growth of herbage. 2) A long-term maintenance of the seasonal frozen soil is good for plant survivor and organism remaining in soil, which migrate with soil freezing and melting. So, the seasonal frozen soil plays an important role for increasing fertility of soil. 3) High water content in soil is also good for the formation of humscd, in turn; the humscd offers some other organism for plant growth. 4) High water content in frozen soil increases the thermal capacity of soil, able to regulate the sequent of climate unusually oscillating. 5) Changing rate of the seasonal frozen soil has an important effect on herbage biomass.
  • LI Ling, ZHU Xi-de, WANG Qing-chun, WANG Zheng-yu
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 320-328. https://doi.org/10.7522/j.issn.1000-0240.2005.0049
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    By using a mathematical statistic methods, geographical information system technology, the space-time evolution of permafrost in Qinghai province is analyzed,and some evidence of permafrost degradation is found. The area of seasonal frozen soils and permafrost is rather wide in the province. The monthly variation of seasonal frozen soils is significant. Usually,the thawing process of permafrost is more complicated than its freezing process,and has a very close relationship with soil characteristics and topographic factors. In the last 10 years,permafrost is in degradation due to distinct increasing of ground temperature, shortening of freezing period,decreasing of the maximum frozen depth,shrinking of permafrost area, enlarging of seasonal frozen soil area, and arising of permafrost base.
  • HAN Hai-dong, DING Yong-jian, LIU Shi-yin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 329-336. https://doi.org/10.7522/j.issn.1000-0240.2005.0050
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    In this paper a simple numerical model is developed to estimate the ice ablation under a debris cover on the basis of heat transfer theory and energy conservation theory. To a given debris cover, three soil thermal layers are classified in the model. Debris layer 1 is characterized by an intense temperature vaxiation and a negative temperature gradient in the nighttime; within layer 2 the temperature is generally changing slowly; debris layer 3 is characterized by a low temperature and a feeble variation of the debris temperature. The model can calculate the temperatures of different interfaces with a given surface temperature, depth and thermal properties of the debris, and then calculate the heat for ice melting. A case study is carried out on the debris-covered area of Koxkar Glacier to the northwest of Tarim basin, to test the model. Three different spots with ice depths of 0.8 m (Spot 1), 1.5 m (Spot 2) and 2.1m (Spot 3), respectively, are selected in the examination. The case study shows that the model is relatively good for the estimation of heat that is consumed for ice ablation. For the debris temperature series of different depths, however, there is still an inconsistency between the simulated and observed values. The main reasons for this inconsistency might be attributed to the improper assumption in the simplified model and the phase lag in the vertical debris temperature profile. Estimation of ablation heat indicates a difference among the three spots. Heat for ablation under a debris cover is 26.87 W·5m-2 for Spot 1, 9.81 W·5m-2 for Spot 2 and 6.92 W·5m-2 for Spot 3, respectively.
  • ZHANG Yong, LIU Shi-yin, SHANGGUAN Dong-hui, HAN Hai-dong, XIE Chang-wei, WANG Jian
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 337-343. https://doi.org/10.7522/j.issn.1000-0240.2005.0051
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    The degree-day method is one of the simplest but sufficiently accurate schemes to estimate ablation on a glacier. It bases on linear correlation between ablation and sum of daily mean temperatures above melting point, which is called the positive degree-day sum (PDD) during a period. The factor linking the ablation to PDD is called the positive degree-day factor. Based on ablation and PDD, the degree-day factors are calculated. The degree-day factors range from2.0 to 9.7 mm 5℃-1·d-1, and its average value is 5.7 mm 5℃-1·d-1. There are some factors influencing the degree-day factors on the Koxkar Baqi Glacier, including altitude, surface condition of the glacier, albedo and terrain. The study shows that: 1) The degree-day factor depends on altitude on the Koxkar Baqi Glacier; in general, the degree-day factor increases as altitude increases, then, the factor at higher altitude is larger than that at lower altitude, which is mainly due to the ablation caused by Absorbed global radiation at the high altitude, where the PDD is low due to low summer air temperature. 2) The degree-day factor of the Koxkar Baqi Glacier decreases as the mean temperature increases, as what observed in Dongkemadi Glacier, July 1 st Glacier, Yala glacier and AX010 Glacier 3) The surface condition of a glacier, including coverage of debris and snow, surface slope, and so on, is an important factor to the degree-day factor on the Koxkar Baqi Glacier. In the ablation area of the Koxkar Baqi Glacier, the zone below 3 900 m a.s.l. is covered with debris, and the zone above 3 900 m a.s.l. is debris-free; the depth of the debris varies from 0 to 250 cm in general. Debris has a strong influence on the surface energy balance and melting of the underlying ice. The surface debris layer works as a good insulator on the Koxkar Baqi Glacier. The factor in the debris-free area is larger than that in the debris-covered area, because of the main physical characteristics of the debris, such as the thermal resistance and albedo, which control the heat conduction to the ice-debris interface. It would be useful to understand the dependence of ablation on degree-day factor in the Koxkar Baqi Glacier, so that one can estimate the contribution of the Koxkar Baqi Glacier melting, using the degree-day method while calculating total discharge from the glacier basin.
  • SHANGGUAN Dong-hui, LIU Shi-yin, DING Yong-jian, DING Liang-fu, SHEN Yong-ping, ZHANG Shi-qiang, LU An-xin, LI Gang, CAI Di-hua, ZHANG Yong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 344-351. https://doi.org/10.7522/j.issn.1000-0240.2005.0052
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    The Glacier inventory of China is the basal data for studying glacier changes. An update of The Glacier inventory of China is necessary, because glaciers in the Northwest China have undergone visible changes under climate warming during the past decades. In this study, the ASTER images are used to investigate the glacier changes in the Muztag Ata and Kongur Tagh. The methods of Crisp, Threshold of a ratio image from ASTER band 3/band 4 and manual interpretation are used to map glacier extent and discriminate glacier zones. The debris-covered glacier zone is classified by overlay DEM and images. The parameters are calculated with semi-automatic and manual approaches to compile the glacier inventory. A comparative analysis performed for glacier area shows that there was area shrinkage of 67.89 km2 from 1962/1966 to 2001, accounting for about 6.2±1.0% of total area. It is demonstrated that it is possible to monitor the dynamic changes of glaciers expediently and rapidly, and to reveal effectively the characteristics of glacier changes by using RS and GIS.
  • ZHAO Qiang, WANG Nai-ang, LI Xiu-mei, CHENG Hong-yi, LI Yu, LI Gang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 352-359. https://doi.org/10.7522/j.issn.1000-0240.2005.0053
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    Investigations of geomorphology and sedimentology, and analyses of radiocarbon dates, grain size, susceptibility, content of carbonate and C/N-indicates of the sediment at the present-day closed basin (Qingtu Lake) in the terminal of the Shiyang River in arid region of China were conducted to recover the history of palaelake change since the Holocene. Qingtu Lake lies in Minqin basin in the east of the Hexi Corridor, which is located in the west edge of the East Asia monsoon. Through a field survey, the profile ZY is chosen as study object. Proxies of the Profile ZY, such as grain size, susceptibility, content of carbonate and C/N, reveal the variation of summer monsoon precipitation in the Shiyang River drainage basin during 9500~1100 a BP. An abrupt event happened during 9500~6700 a BP, when climate was droughty and windy, with sands depositing; During 6700~5800 a BP summer monsoon strongly impacted the region, and precipitation was abundant, atmosphere was humid, lakes were deeper; During 5800~2700 a BP summer monsoon became unsteady, so was water level of lakes, with frequently fluctuating climate; During 2700~1100 a BP human activity increased obviously and water level of lakes declined continuously, so it is necessary to study whether the natural factors were the key to control the water level.
  • XU Bai-qing, YAO Tan-dong, LIU Xian-qin, GUO Xue-jun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 360-367. https://doi.org/10.7522/j.issn.1000-0240.2005.0054
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    Ice cores methane reconstructions are believed to reflect atmospheric CH4 concentration fluctuation with time and to reveal the past changes in terrestrial methane emissions. It has been proposed that the past natural CH4 fluctuations were mainly due to changes in the source strength, through variability of the wetland extent in tropical regions. This was partly confirmed by the combined analysis of ice cores from Greenland and Antarctica, allowing quantifying the difference of mixing ratio between the two Polar Regions with time. For the most recent time (last 1000 years), these data suggested that tropical sources became more important, potentially due to the already significant contribution of human-induced sources. Still, this analysis of available CH4 data from Greenland and Antarctica relied on several critical assumptions, among them that the CH4 sources between 30°S and 90°S remain unchanged with time. The lack of constrain on the CH4 mixing ratio in tropical regions appeared as the major caveat in this exercise. This work has thus put an urgent task in reconstructing CH4 concentration from the low and mid-latitude areas, based on ice cores drilled at very high altitude in mountain glacier. The Dasuopu ice core provides a unique opportunity for obtaining sub-tropical latitude CH4 reconstruction, because of its high altitude (7000 m a.s.l, making it the highest-ever drilled site in the World), which provides low ice temperature and limited summer melting, so that the original CH4 concentration has a good chance to be preserved.;The Dasuopu record shows an obvious CH4 concentration increase in the low-mid latitude since industrialization, and reveals similar trend of methane concentration fluctuation with the polar region records. This sub-tropical CH4 record also allows quantifying for the first time the difference of CH4 mixing ratio between polar and sub-tropical latitudes during pre-industrial time. The average CH4 concentration in the record from the Dasuopu ice core is 782 nmol 5mol-1 in the time interval of 0~1850 AD, and the maximum temporal variation exceed 220 nmol 5mol-1, which has never been found in polar ice records. The average difference is 66 nmol 5mol-1 with Greenland and 107 nmol 5mol-1 with Antarctica. The record suggests that the tropical latitudes might represent as much of the global CH4 sources in pre-industrial time.;The last low concentration period in CH4 appeared around 1790 AD. Since 1850, there has been a record increase in CH4. Although some polar ice cores seem recorded a very early start (1750 AD) of anthropogenic input of CH4, it is difficult to see this in the Dasuopu ice core. In the Polar Regions, the study of Rasmussen and Khalil concluded that a rapid and significant CH4 concentration increase started about 150 years ago, which is consistent with the results here. It is also found that the CH4 concentration in the atmosphere 150-year ago was about 45% of present level and was not significantly influenced by human activities.
  • LI Jian-dong, BIAN Lin-gen, GAO Zhi-qiu, LU Long-hua, LU Chang-gui
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 368-375. https://doi.org/10.7522/j.issn.1000-0240.2005.0055
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    Friction velocity, sensible and latent heat fluxes are measured using aerodynamic profile and bulk transfer methods with different universal functions for the surface meteorological data collected in drifting ice area during the Chinese Second Arctic Research Expedition, August 23 to September 4 in 2003. The results show that Holtslag universal function is much better than other universal functions mentioned in this study for calculation of fluxes. The turbulence fluxes at different levels obtained by bulk transfer method satisfy the constant flux hypothesis in surface layer better than that by profile method. Hopefully, it gives important support for further improving boundary layer parameterization at Arctic drifting area.
  • ZHANG Guang-xing, YANG Lian-mei, YANG Qing
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 376-380. https://doi.org/10.7522/j.issn.1000-0240.2005.0056
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    Based on the daily observational data from 1960 to 2002 from 11 air sounding stations located in the western slopes of the Altay Mountains, northern slopes of the Tianshan Mountains, southern slopes of the Tianshan Mountains, northern slopes of the Kunlun Mountains and the western regain of North Xinjiang, respectively, the changing trend and the difference of spatial distribution of the average height of 0℃ level in summer in Xinjiang were analyzed for the 43 years, according to the features of climate and runoff. By means of Mann-Kendall method, abrupt test was conducted. The results showed that there was an increasing trend of the 0℃ level height as a whole: In the 1960s it dropped obviously and then became relatively smooth in the 1970s. However, it rose from the 1980s, especially in the early 1990s it rose more obviously. But there was no significantly abrupt climate change. It increased gradually from south to north and from west to east in Xinjiang, with an exception of the southern slopes of the Kunlun Mountains. The increasing from the 1980s up to now was the common trend, with a local difference. The 0℃ level height increase indicated that the temperature at the lower level of the upper air is increasing. It is demonstrated that there is a climate change in the upper air as well as on the surface. Meanwhile, the increasing trend goes with precipitation increase, glacier shrinkage, river runoff increase and lake level rise in Xinjiang.
  • LI Xia, REN Yi-yong, TANG Hao, CHEN Hong-wu
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 381-388. https://doi.org/10.7522/j.issn.1000-0240.2005.0057
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    The changes of water resources and the reasons which cause the changes over the middle Tianshan Mountains between 42.5 N and 45.0 N,and 85.0°E and 90.0°E were analyzed by using observed data of 17 meteorological stations during the past 40 years and monthly mean data provided by NCEP/NCAR from 1950 to 2000. In this area the annual mean precipitation was gradually going up and increasing obviously in summer and winter. At the same time, the increase in annual mean precipitation of mountain areas was more than that of the surrounding plains. Mean decadal precipitation of 17 stations came down form the 1960s to the 1970s, but went up from the 1980s to the 1990s. Moreover, the precipitable water showed an increasing trend. In the atmosphere over the area of 2.5×5.0, the annual influent water vapor amount was 9217.8×108 m3, the annual effluent water vapor amount was 8625.7×108 m3, and annual net water vapor amount was 592.0×108 m3, averaged over the past 50 years. The influent water vapor amount in summer mainly contributes to annual net water vapor amount. Only 6.4% of annual influent water vapor amount contributed to precipitation, which was lower than that of the China mainland. The water budget was inclined to reduce from the 1950s to the 1990s but slightly increased in the 1990s. Considering runoff goes up and glaciers retreat, it is thought that one reason to cause the rainfall increasing over the middle Tianshan Mountains is the increase of the locally circulatory water amount and the locally circulatory frequency.
  • YANG Lian-mei, YANG Tao, JIA Li-hong, CHANG Tao
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 389-396. https://doi.org/10.7522/j.issn.1000-0240.2005.0058
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    Based on compiled daily rainfall data from 50 meteorological stations in the northern Xinjiang Region and the Tianshan Mountains from November 1st to April 15th of the next year between 1961 and 2002,the spatial and temporal distribution characteristics,interannual variation of heavy snowstorms are analyzed by the methods of statistics and diagnose. The causes of severe snow disaster during 2000-2001 winter are analyzed, and the origin and the characteristics of the water vapor of heavy snowstorms are studied through a typical example. The results show: 1) There are 4 high frequent areas, namely Altay area, Tachen basin, Yili valley and north slopes of Tianshan Mountains from Wusu to Mulei; Heavy snow processes in the first three regions are over 50% in previous winter, and in spring and middle winter in turn, and about 43% in north slopes of Tianshan Mountains during previous winter and spring. 2) Heavy snow processes exhibit an obvious increase in Altay area (0.3 times 5(10a)-1), Yili valley (0.7 times 5(10a)-1) and northern Tianshan Mountains (0.5 times 5(10a)-1). 3) Heavy snow processes are abnormal less before the 1980s, abnormal more after the 1980s, mainly in the 1990s. 4) Severe snow disaster during 2000-2001 winter was caused by persistence abnormal atmospheric circulation and frequent cold air and many snowfall processes. Water vapor depends on atmospheric circulation, and it is brought by north cold air, westerly wind in middle latitude and southwest wind in low latitude. Vapor transfer in 700 hPa is equivalent to that in 850 hPa, and that in 500 hPa cannot be ignored.
  • YANG Qing, CUI Cai-xia
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 397-403. https://doi.org/10.7522/j.issn.1000-0240.2005.0059
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    To reveal the changing trend and annual distribution traits of the surface water and climate elements in the Bayanbuluk alpine-cold wetland in the last 50 a, temperature, precipitation, different rank precipitation days, evaporation, water vapor pressure, relative humidity, dust storm days, snow depth etc. were used to analyze their change trends. No distinct warming trend of annual mean temperature and no obvious changing of the annual maximum or minimum temperatures can be seen, no matter in winter or as a whole. However, there is an increase in mean temperature in summer, which is higher in the Bayanbuluk alpine-cold wetland than in other areas of the Xinjiang Region. Precipitation in summer is the main water source in this wetland and accounts for 68.4% of the total. Precipitation in the mid 1980s dropped to the lowest during the last 50 a, and then increased gradually. Also the runoff of Kaidu River has increased since 1987, with a nice linear response relationship with the precipitation and annual temperature in the Bayanbuluk alpine-cold wetland. The impact of climate change on surface water environment associates directly with the ecosystems in this area.
  • YU Shu-long, YUAN Yu-jiang, JIN Hai-long, CUI Yu, LIU Bin, LIN Chun-liang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 404-410. https://doi.org/10.7522/j.issn.1000-0240.2005.0060
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    Single correlation calculation indicated that the correlations were significant among two tree-ring chronologies and precipitation from July to August on the midwestern part of the northern slopes of Tianshan Mountains, with a maximum correlation coefficient of 0.639 (α=0.00002). In consideration of that tree-growth variation lags behind precipitation variation, a 379-year precipitation series was well reconstructed, with an explain variance of 56.0%. It was verified that the reconstructed precipitation series was reliable. Analyzing the 379 year reconstructed precipitation series found: 1) There were significant change periods of 6.6, 6.5, 5.4 a; 2) There were 5 abrupt changes in 1734, 1759, 1819, 1872, 1963; 3) There were 6 wet periods and 6 dry periods. The change of the reconstructed precipitation series consists well with that of the precipitation series in Yili Prefecture.
  • YUAN Yu-jiang, YU Shu-long, MU Gui-jin, CHENG Fa-hu, GONG Yuan, LIU Bin, ZHU Yun-chuan, GUO Jian-guo
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 411-417. https://doi.org/10.7522/j.issn.1000-0240.2005.0061
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    Correlation analyses show that correlation between the series of the tree-ring chronologies from the Basin of Manas River and the annual runoff at Kensiwate Hydrological Station of the Manas River is significant and the best single correlation coefficient is 0.524, with a significance level of 0.0002. Using five series of tree-ring standard chronologies, a 355-year series of annual runoff can be reconstructed for Kensiwate Hydrological Station of the Manas River on the north slopes of Tianshan Mountains, with an explained variance of 61%. Verification from statistical parameters and independent reconstructed runoff data shows that the series of annual runoff reconstructed for the past 355 years is reliable. Analysis of the 355-year reconstructed runoff features indicates: 1)There were 11 periods below long-term mean and 10 periods above long-term mean. Among them, the longest period above mean was from 1670 to 1699, lasting 30 years, and the longest period below mean was from 1949 to 1994, lasting 46 years. 2)There were two drying periods with the highest significance, lasting more than 100 years, from 1872 to 1995 and from 1671 to 1775, with runoff decreasing rates of 0.19?108 m3·(10a)-1 and 0.26?108 m3·(10a)-1, respectively. 3)There were two abrupt changing periods from 1711 to 1712 and in 1872, the former changing from more to less, but the latter changing from less to more. 4)There were two rich-water decades in the 1660s and the 1670s, with a runoff of 17.9~18.1% more than that at present (the mean is 12.19?108 m3 from 1956 to 2000), and one short-water decade in the 1860s, with a runoff 16.7% less than that at present. 5)The reconstructed runoff has 58~59, 9.6, 27.2, 16.9, 4.8, 4.3, 2.9~3.0 years variation quasi-periods.
  • GU Xiao-wei, LI Guang-jun, WANG Qing, LIU Jian-xing, DING Yi, LIU Jing-zhi
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 418-425. https://doi.org/10.7522/j.issn.1000-0240.2005.0062
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    The principles of the componential method for ecological footprint calculation are introduced and its mathematical model formulated. The method is then applied to case studies of university campuses to investigate the ecological efficiency of high education. The ecological footprints of two university campuses, Northeastern University (NEU) and Shenyang University (SYU), were calculated and analyzed for the year of 2003. The components considered in this study include energy (coal, natural gas and electricity) consumption, food consumption, waste disposal, water supply, transportation, and paper consumption. The ecological footprint of NEU was 24787 hm2, which means that nearly 25000 hm2 of ecologically productive land was needed to support the consumptions and to Absorb the wastes from the campus for that year. The ecological efficiency of NEU was 0.94 student/ha. The ecological footprint of SYU was 17218 hm2 with an ecological efficiency of 0.8 student/ha. It can be seen that one hectare of land with the global average productivity is not sufficient to support a single student at NEU or SYU. The largest footprint component for both NEU and SYU is from energy consumption, which takes up 68% and 54% of the total footprints of the two universities, respectively. The second and third largest footprint components are from food consumption and waste disposal. Reducing energy consumption and waste generation is, therefore, crucial to reducing the footprints and thus making the campus ecologically efficient.;The student consumption power has a significant effect on the total footprint and eco-efficiency of the campuses. The higher is the per student consumption, the lower the eco-efficiency. The student consumption level is in turn determined by the average per capita income of the student families. Preliminary investigations reveal that there exist pronounced differences in the student income situation between the two universities. NEU has more students from remote and rural areas where the economy is less developed than from cities; some 30% of the students of NEU are from low income families; 10%~15% from very low income families and above 5% from extremely low income families. On the contrary, most students of SYU are from city families whose income is much higher than those of NEU. The effect of this difference in family income and, thus, in on-campus consumption can be clearly seen from the composition and proportion of the footprint from food consumption (Table 2). The per student consumption of meat at SYU is twice as high as that at NEU, and consequently, the footprint proportion from food consumption at SYU is higher than that at NEU (37.5% vs. 21.8%). The student income situation is one of the main factors causing the eco-efficiency of SYU (0.80 student/ha) lower than that of NEU (0.94 student/ha).;The disciplinary areas and the intensity of research activities also have a significant effect on the ecological footprints of university campuses. This effect is mainly reflected on the footprint of electricity. The main disciplinary areas of NEU are in Engineering and Technology while those of SYU in social sciences and, hence, the former has many more laboratories with relatively heavy equipments than the latter. Also, NEU is research oriented and its intensity of research is much higher than that of SYU, which is, teaching oriented. As a result, the per student electricity consumption at NEU is 1.75 times as high as that at SYU, and the footprint component associated with electricity takes up a much higher proportion of the total footprint at NEU than that at SYU (13.5% vs. 6.5%).;A comparison of the ecological footprints of NEU and SYU of China and Redlands University (RU) of Australia reveals that the level of economic development has significant impacts on the total footprint, the proportions of footprint components, and the eco-efficiency of a university campus. Australia, being an industrial nation, has a much higher level of economic development than China who is a developing country.This difference is reflected on two components: energy and transportation. The Australia university does not use coal on campus; the foot prints corresponding to its electricity and transportation takes up 31% and 32%, respectively, of the total foot print, which are several times higher than the corresponding foot print proportions of the two Chinese universities (Table 6). This study provides, quantit atively, an in sight into the ecological implications of high education and demonst rates that Ecoogical Foot print can serve as a practical and meaningful tool for comparing and monitoring the sustainability of university campuses.
  • LUO Zhen-li, HUANG Huang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 426-431. https://doi.org/10.7522/j.issn.1000-0240.2005.0063
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    Agriculture is the most important sector of water use; water content in agricultural products is high. Water used in the production process of an agricultural/industrial product and service is called virtual water. Based on the developing characteristics of major agricultural products in Chenzhou, Shaoguan and Ganzhou of the Red Triangular Region, an quantitative analysis on virtual water of main water-consumed agricultural products in 2000 is made, and some suggestions are put forward on how to adjust the structure of agricultural products and to utilize the water advantage in the Red Triangular Region. As to virtual water consumption per capita of agricultural products of the urban residents, there are obvious gaps among the three studied cities; it is higher in Shaoguan than in Chenzhou or Ganzhou. Under the precondition without cutting down the average water consumption, those areas with abundant water resources can take the advantage of export of virtual water of agricultural products. In other water-short areas, it is necessary to adjust the strategy of agricultural products, to develop high-efficacious agriculture and to import the agricultural products of more water resources in order to alleviate the press of water shortage. It is an innovation of the regional resource management.
  • ZHOU Chen-chao, JIA Shao-feng, YAN Hua-yun, YANG Gui-lin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 432-437. https://doi.org/10.7522/j.issn.1000-0240.2005.0064
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    In this paper the changing trend of water resources in Qinghai Province is studied. The main representative stations in the head area of the three big rivers (Yangtze River, Yellow River, and Lancang River) are selected. Mann-Kendall and Lineal-Correlation methods are applied to analyze the changing trends of hydrologic components. By use of the yearly series of natural runoff and precipitation data acquired from the representative stations (1956-2000), it is found that the changing trend of water resources in the head area of the three rivers is different from what achieved before. The results calculated by the two significance test methods are both below the standard value, which confirm the changing trend of water resources in Qinghai Province is not obvious. The water resources did not show an obvious variation trend in the past 45 years; however, it is found that the natural runoff has decreased since 1990. The water shortage in the 1990 had taken some bad influence to Qinghai s environment. At the same time, in order to explain the argument from more expansive area in Qinghai Province, three stations are selected from the areas of internal drainages to analyze. From the analysis, the same result is achieved as what achieved from the previous stations, except for Xiangride station. Of the variation of water resources in the areas of internal drainages, also no any obvious changing trend can be seen. But in Xiangride Station, it is found that both precipitation and natural runoff are obviously increasing.
  • ZHANG Xin-bao
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 438-443. https://doi.org/10.7522/j.issn.1000-0240.2005.0065
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    The shapes of depth distribution profiles of fallout 137Cs, which were produced by nuclear weapon testing during the period of 1950-1970, are different in the deposits between non-glacial and glacial lakes. As fallout 137Cs with a short half life of 30.17 a in modern lake deposits, depth distribution shapes of cosmogenic radionuclide 10Be with a long half of 1.5 Ma should be different in the deposits between glacial and non-glacial lakes during Quaternary period. For a glacial lake, the amounts of accumulated ice layers and the containing 10Be radionuclide are greater than the delivering values by meltwater over the catchment in glacial periods, while the amounts are less the delivering values in inter-glacial period. The fluctuations of 10Be concentrations in deposit profiles of glacial lakes may reflect the changes of ice accumulation and melting during the quaternary period. For non-glacial lakes, there are no such effects of ice accumulation and melting on the 10Be delivering yields from the catchment exist during the Quaternary period. A comparative study on 10Be in deposits between glacial and non-glacial lakes may have great potential for solving the century s debate on the paleo-glaciers in the eastern low-middle mountain regions and on the ice sheet in the Tibet Plateau of China.
  • SUN Chao
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 444-448. https://doi.org/10.7522/j.issn.1000-0240.2005.0066
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    The sediment deposit and the rising of the channel bed are the key problems of the Lower Yellow River. Severe soil erosion from the Loess Plateau where the upper reaches of the Yellow River traverses has accumulated by big amount at the lower reaches of the river, making the riverbed elevated by annual rate of 0.1 meters, and now the watercourse is four to six meters higher above ground level for about 800 kilometers in the lower reaches. The capable of water flow in channel of the lower Yellow River have greatly reduced from 5000 m3 per second in1980s to 2000~3000 m3 per second due to sediment deposit and the rising of channel bed.;From the history of the Yellow River, we know that the Yellow River flowed through the north side of the current channel before the year 1128 into the Bohai Sea in Tianjing. From 1128 to 1855, the Yellow River flowed through the south side of the current channel, passing the Huaihe River into the Yellow Sea. After the breach at Tongwaxiang, the Yellow River flowed along the current channel into the Bohai Sea. The current channel from Dongbatou to Zhengzhou is the old channel of the Ming dynasty and the Qing dynasty which has a history of more than 500 years. In the section between Dongbatou and the estuary, the flow spread after the breach in 1855 without man-made dikes. In 1877, the government built the dike based on the levees built by local residents after 22 years of overflow. The channel change and sediment deposit are result in the geological process. The prediction of the channel dynamics should be desiderated in the Yellow River harness in future.
  • XIN Ping
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 449-453. https://doi.org/10.7522/j.issn.1000-0240.2005.0067
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    Base on the analyses of the destroyed types and mechanisms of the National Highway 213 from Hezuo to Langmusi, which lies in a seasonal frozen soil region, the engineering techniques for solving frost heaving and frost boiling of embankment in the rebuild engineering are proposed. The average altitude of the highway is about 2950~3620 m a.s.l. Meteorological data show that the maximal frozen depth in this area is 1.42 m. There is a large amount of soft soil, such as humus soil and black land along the highway, as well as swamp, which damage the way construction and operation. The original way had suffered heavy damages from cold weather and bad engineering geological conditions. In the rebuilding engineering of the highway 213 from Hezuo to Langmusi, designers adopted some engineering techniques in accordance with the engineering conditions of different sections of the way. Replace-filling embankment with gravel and riprap for extruding silt are built. Geotextile is also used to strengthen the embankment and obstruct moisture into the embankment. Practice shows that the engineering techniques are effective in preventing frost heaving and frost boiling of embankment. These techniques are also applicable to the areas of similar condition.
  • JIN Hui-jun, YU Wen-bing, CHEN You-chang, GAO Xiao-fei, LI Fu-qing, YAO Zhi-Xiang
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 454-464. https://doi.org/10.7522/j.issn.1000-0240.2005.0068
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    With the rapid development of oil pipeline technologies, the length, diameter, construction difficulty, complicity and risks of pipelines in permafrost regions have been increasing steadily. Some key oil pipelines have to traverse extensive expanse of permafrost, which provide great challenges for engineering deign and construction. The key issues in the engineering stability of oil pipelines are frost heave and subsequent thaw settlement in permafrost foundations. Therefore, design and construction in cold regions have to carefully consider the impacts of topography and environments on frost heave and thaw settlement, and their impacts on the engineering foundations and the integrity of pipelines. The environmental movements since the 1960s have greatly influenced the design and construction of oil pipelines in cold regions, which further complicated the issue, but also facilitated the research programs on these issues.;The success of the Trans-Alaska Oil Pipeline are attributed to the substantial investments in research and experiments, sufficient time for project evaluation, debating, and decision-making, as well as extensive participation of the public. The solutions of the permafrost problems include series of creative and innovative designs for reducing thaw settlement and environmental damages. The key scientific questions are focused on the impacts of the heated pipeline on the thermal and moisture regimes of permafrost, among which the most dangerous hazards would be potential differential thaw settlement and its impacts on pipeline deformation and integrity. The secondary hazards include the changes of micro-topography, drainage and vegetation after the construction of the pipeline, and the possible damages of the induced thaw settlement on pipeline stability and its ambient eco-environments. The 17-year observations on the temperatures, thaw penetration and surface thaw settlement within the right of way (ROW) regions and undisturbed sites along the Norman Wells Oil Pipeline indicate that the thaw penetration is still within the design predictions while the surface settlement in the trench in organic and ice-rich mineral soils has reached or exceeded design predictions in some locations. Along the Golmud to Lhasa ambient temperature product pipeline, frost heave and thaw settlement, as well as worn out, damaged or inadequate cathodic protection, and natural hazards such as strong earthquakes and flash floods have caused significant deformation of pipes and leaks many times during the past 28 years, necessitating a major renovation. Most of the frost heaving and thaw settlement occurred in ice-rich, fine-grained lacustrine sediments with shallow water table.;The observations and unique long-term data sets on oil pipeline engineering have greatly increased the body of knowledge in geocryology. They have supported the modification of operations, mitigation of frost hazards, and formulation of emergency response measures. In these studies, permafrost researchers, cold regions and pipeline engineers and project decision-makers need to discover, fully understand and correctly forecast potential problems as soon as possible, through careful investigations, close cooperation and mutual trust. If designed properly and the construction closely followed the designed specifications, all these problems would not necessarily produce significant consequences.
  • CHANG Xiao-xiao, MA Wei, LAI Yuan-ming, SHEN Ying
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(3): 465-468. https://doi.org/10.7522/j.issn.1000-0240.2005.0069
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    The Triaxial Material Test Machine of MT’S-810 set in the State Key Laboratory of Frozen Soil Engineering was manufactured in the 1980’s and controlled by mode of simulation signal. Now it is upgraded and improved. The principle is to replace the simulation control system with a digital control system with many channels. Thus, the capacity, precision and automatization level of the machine is improved greatly, and its service life will be prolonged.