25 October 2005, Volume 27 Issue 5
    

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  • LI Shu-xun, WU Tong-hua
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 627-632. https://doi.org/10.7522/j.issn.1000-0240.2005.0093
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    Multivariable linear regression has been applied to analyze the recorded data of annual mean air temperature and annual mean ground temperature from 119 meteorological stations from 1991 to 2000 in the Tibetan Plateau.The linear statistic coefficients between monthly mean air temperature,monthly mean ground temperature and latitude,longitude and elevation in the research region are obtained.It is demonstrated that the air temperature,ground temperature and their annual ranges in the Tibetan Plateau are highly correlated with corresponding latitude,longitude and elevation.It is indicated that the air temperature and ground temperature in the plateau can be expressed as functions of location coordinates and time.Taking the validated statistic results of annual mean air temperature and annual mean ground temperature from 1991 to 2000 as the experimental results between air temperature and ground temperature,it will contribute to the determination of upper boundary condition of permafrost at any time and any site.These results are of great significance to under-construction Qinghai-Tibetan Railway and to the prediction of permafrost environment.
  • WANG Yi-bo, WANG Gen-xu, SHEN Yong-ping, Wang Yan-li
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 633-640. https://doi.org/10.7522/j.issn.1000-0240.2005.0094
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    The grassland environment in the cold regions of the Tibetan Plateau is an important parts of the tableland environment,because of the influence of the natural environment changes and the disturbances from the human activities;the meadow environment of the tableland is in great degradation now.In a representative area in the degraded meadow,the changes of the soil moisture in the grassland,the edaphic structures and the status of the vegetations are studied.It is revealed that after the grassland degradation,the courses of the soil moisture have changed a lot,and the more vegetation degenerates,the more soil moisture changes,and the process of the water entering into soil also becomes quick.Then, the succession of communities become more distinct,the preponderant plant degenerates greatly,and the plants become small.The soil erosion becomes heavy than ever and in the arid regions,desertification becomes more serious.The natural disasters,including the pests from rats and insects,will be frequent.
  • SHANGGUAN Dong-hui, LIU Shi-yin, DING Yong-jian, DING Lian-fu, SHEN Yong-ping, LU An-xin, LI Gang, ZHANG Yong, XIE Chang-wei
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 641-644. https://doi.org/10.7522/j.issn.1000-0240.2005.0095
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    There is little information about Glacier surging in China.In this paper,the Chinese Glacier Inventory,Landsat MSS/TM/ETM+ and historical map are used to obtain the extent of Glaciers 5Y654D48 and 5Y654D97,which are located in the Shaksgam River in Karakorum Mountains,in 1968/1976,1977,1990 and 2000/2001. A comparative analysis for the glacier extent was employed to discuss the annual flow velocity of the two glaciers.The velocity for the Glacier 5Y654D48 was 272 m·a-1 during 1990-2000,and for the Glacier 5Y654D497 was 213 m·a-1 during 1977-1990,respectively.They were 7~20 times the annual mean velocities of the two glaciers in other periods.It is found from the abnormal ice flow velocity that the Glacier 5Y654D48 was surging during 1990-2000 and the Glacier 5Y654D97 was surging during 1977-1990.
  • ZHANG Shi-qiang, DING Yong-jian, LU Jian, LIU Shi-yin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 645-648. https://doi.org/10.7522/j.issn.1000-0240.2005.0096
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    Water-heat process in the Tibetan Plateau is significant to global change,and soil moisture and soil temperatures are the key factors of simulating water–heat process.In this paper,a water and energy balance macro scale hydrological model was used to compare the simulated with observed at the step of 1 hour during 399 days in Tuotuohe.The results of meadow evaporation,short-wave radiation, and net radiation were discussed.It is revealed that the evaporation of alpine meadow is the main part of total evapotranspiration of alpine meadow.The total evaporation all the year round is equal to that observed in the Urumqi River area.The simulated daily short-wave radiation is in some sort greater than that observed in winter,whereas the simulated daily short-wave radiation is nearly equal to the observed one,and the fluctuation in a day of simulation is less than that of observation due to daily precipitation input in summer.The simulated yearly net radiation is near to the research result of reference[12].
  • ZHANG Jie, HAN Tao, WANG Jian
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 649-654. https://doi.org/10.7522/j.issn.1000-0240.2005.0097
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    By using NOAA-AVHRR and EOS-MODIS data from May to August,1997-2004,spectrum characteristics of snow and ice are judged and analyzed,statistics of snow-cover area of three basins in the Qilian Mountains are made,and,by analyzing 8-year precipitation and altitude data,the snowline latitude-dependence is found.The result shows that the variation of snow-cover area from Jun to August was small,but it was large in May in the middle and east of the Qilian Mountains;on the contrary,temperature of snow-cover region was increasing,except for May;there was an increase in total precipitation of the Qilian Mountains from May to August.It is revealed that snow-cover area and snow line altitude change obviously with climate change of global and region,especially,in the middle section of the mountains.By analyzing artificial snowing data,it is demonstrated that artificial snowfall operation has a certain buffer function to snow ablation.
  • HAN Tian-ding, YE Bai-sheng, DING Yong-jian, JIAO Ke-qin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 655-659. https://doi.org/10.7522/j.issn.1000-0240.2005.0098
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    Based on the observations of runoff and precipitation in the Ürüqi River basin,the variation features in climatic shift from warm-dry to warm-humid are analyzed.It is reveals that there is an obvious increasing trend of runoff at the Glacier No.1 and Yingxunqiao Hydrologic Stations of the Ürüqi River after 1987.Especially,the runoff at the Glacier No.1 Hydrologic Stations has a very clear shift in 1997.The main reason of the increasing runoff is the obvious increment of precipitation in the source area of the Ürüqi River.Doubtless,the shift of glacial runoff in the Glacier No.1 Hydrologic Station is due to the two factors: strong ablation of glacier and durative increase in precipitation.
  • LIU Yu-lian, WU Hong-bao, LI Dong-liang, SONG Li-hua, SHEN Yong-ping, ZHANG Jian, LIU Xue-hua
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 660-665. https://doi.org/10.7522/j.issn.1000-0240.2005.0099
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    The series of monthly mean temperature anomaly for the recent 94 years in Harbin is analyzed with SSA.Results show that there is a general warming of about 1.54℃ for the whole period,with a warming of about 0.53℃ from 1918 to 1952,a warming of about 1.03℃ from 1971 to 2002 and a cooling from 1962 to 1970.Moreover,there is also a quasi-12-month oscillation periods,showing that the cycle also had an apparent decadal-scale variety from 1909 to 2002: monthly mean temperature in winter time from 1984 to 2002 was about 2.3~3.7℃ warmer than that from 1909 to 1931,while in summer it was about 0.2℃ colder,and the seasonal cycle from 1932 to 1983 was approximate to the mean level of the 94 years.Also,the maximal increase of air temperature in the recent 20 years in Harbin is in February or March.
  • CHANG Zong-qiang, FENG Qi, WU Yu-xia, SU Yong-hong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 666-672. https://doi.org/10.7522/j.issn.1000-0240.2005.0100
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    In the Qilian Mountains,sub-alpine scrub forestis the main vegetationtype and coversabout 42.58% of the total land area.Understanding of the sub-alpine scrub forestefflux of CO2 from the soil surface is a key component of the carbon balance of its ecosystem.Quantifying this flux and understanding the factors,which control the variation of temperature and soil moisture,are fundamental to understand the behavior of the ecosystem as a whole and to predict the consequences of climate change.Soil surface CO2 effluxes were measured on early April to late October 2004 witha LiCor 6400 gas exchange analyzer with soil respiration chamber attachment(LiCor Inc.,Lincoln,NE,USA).The analyzer is a closed infrared gas onethat measures soil respiration.FivePVC collars(0.008 m2) areinstalled randomly a 5m 5m area,and the soil respirationwas measured continuously3 daysper month.Collars were imbedded approximately 2 cm into the soil and left in place throughout the measurement period.It wasnot measure until 1 week after installation to minimize the effects of disturbance from collar installation.And removed live vegetation inside the chamber collars at least 24 hr before measurements to minimize the influence of soil disturbance and root injury on the measurement.To evaluate the statistical models for estimating soil CO2 efflux,soil temperature and soil water content were measured.Soil temperature was measured at 15 cm by a probe attached to the IRGA chamber,and then a temperature profile was measured.Soil water content was measured by using time domain reflectometry(TDR;Tektronix cable tester) at each plot during the soil chamber measurements.During the growing season,the diurnal variation of meadow soil respiration in the mountain watershed of the Heihe River basin was low at night,with the lowest at 2:00~6:00,and started to rise rapidly during 7:00~8:30,and then descended during 16:00~8:30.The maximum soil CO2 efflux appeared during 11:00~6:00.The maximum of average soil CO2 efflux occurredin July and August,followed by May and September,and then by April and October.And it was basically consistent in April and October.The diurnal average of meadow soil CO2 efflux was between(0.79±0.60)μmol·m-2·s-1 and(2.49±0.97)μmol·m-2·s-1.Temperature,soil moisture and vegetation had great effects on the spatial variation of soil respiration in the area.
  • MA Wei-qiang, MA Yao-ming, LI Mao-shan, Z.Bob SU, WANG Jie-min
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 673-679. https://doi.org/10.7522/j.issn.1000-0240.2005.0101
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    It is very important to study the regional heat fluxes in the Tibetan Plateau Area.Using CAMP/Tibet(CEOP,Coordinated Enhanced Observing Period) Asia-Australia Monsoon Project(CAMP) on the Tibetan Plateau(CAMP/Tibet,2001-2005)) data,land surface heat fluxes are analyzed.Those are the net radiation flux(Rn)、sensible heat fluxes(H)、latent heat fluxes(E) and soil heat fluxes(G0).Some new results are gotten in the Northern Tibetan Plateau.1) In the Tibet plateau,the yearly variations of downward shortwave and long-wave radiation,upward shortwave and long-wave radiation,net radiation fluxes are clearly,its July numerical values are larger than January.Their eigenvalueas are 230,245,53,345 and 95 W·m-2;2) In the Tibetan Plateau,the diurnal variations of net radiation,sensible,latent and soil heat fluxes are clearly.They increase with the increasing of solar altitude angle after the sunrise in the morning,and the maximum appears around the noon then they decrease with the decreasing of solar altitude angle.3) Latent heat flux is the main point in summer and sensible heat flux is the main point in winter.In June latent heat flux and sensible heat flux is almost equality.At the beginning of July the latent heat flux is the main aspect until September,then sensible heat flux is the main aspect until the coming year if May.4) The variation of soil heat flux is slow and its value is very small.
  • JIANG Hao, WU Qing-bai, WANG Ke-li, ZHANG Li-jie, FENG Wen
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 680-685. https://doi.org/10.7522/j.issn.1000-0240.2005.0102
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    Based on the field observation data,the atmospheric radiation flux parameterization schemes in the thermo-dynamic model of the ground surface and embankment surface along the Qinghai-Tibet railway are made and used to process the solar direct radiation flux,atmospheric diffuse radiation flux and downward long-wave radiation flux,and the results are good.In the cloud free condition,the parameterization schemes are made for the direct solar radiation flux with permeation ratio and for atmospheric diffuse radiation flux with solar zenith angle,and for the atmospheric downward long-wave radiation flux with atmospheric equivalent emissivity and air temperature.In the cloudy condition,there are the better effect of the cloud amount parameterization scheme based on the cloud cover ratio for generic instantaneous circs and the cloud coefficient parameterization scheme based on the climate data for climatic mean circs.The parameterization for the soil heat flux and the surface drag coefficient are discussed,and the more perfect method needs to combine further with measure experiments.
  • LI Ning, WEI Qing-chao, WEI Jing
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 686-693. https://doi.org/10.7522/j.issn.1000-0240.2005.0103
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    The experimental project of air-cooled riprap subgrade and common subgrade was designed and performed in the Qingshuihe Test Field,an area of warm permafrost with fine frozen soil along the Qinghai-Tibet Railway,to determine the temperature field of the subgrade after the railway construction.Based on ground temperature and deformation monitoring in two freezing-thawing cycles of two sections,ground temperature variations of natural hole,left and right shoulder’s holes,the maximum thawing depth,and the deformation in these two kinds of subgrade were analyzed comparatively.It is revealed that the air-cooled riprap subgrade had better effect of lowing ground temperature,lifting the maximum frozen-thawing depth obviously and decreasing deformation,as compared with the common subgrade.Therefore,the air-cooled riprap subgrade was a positive frozen soil protection measure for its effectively decreasing ground temperature and protecting permafrost.
  • WEN Zhi, SHENG Yu, MA Wei, WU Ji-chun
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 694-700. https://doi.org/10.7522/j.issn.1000-0240.2005.0104
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    In many cases,protecting permafrost from further thaw due to human activities might be the first choice for embankment design in permafrost regions.2-D finite element analysis of temperature field with phase change is conducted to simulate the thermal state of the Qinghai-Tibetan railway with extruded polystyrenes (EPS).Based on the predicted maximum thawing depth for the following 50-year,the rational position,width and thickness of the insulation,whose construction season,and the applicable range of the insulation in embankment engineering of the Qinghai-Tibetan railway in terms of mean annual air temperature(MAAT) were discussed. Numerical results show that 10 cm EPS is an appropriate choice considering economy and intensity.Moreover,the deeper the insulation is placed,the better the thermal-insulation efficiency is.Constructed season affects the maximum thawing depth of embankment.Considering the difficulty in cold climate,embankment with insulation may be constructed before thawing or after freezing.The wider the insulation is,the better the thermal-insulation effect is.As for permafrost regions along the Qinghai-Tibetan railway where MAAT is from-4.00℃ to-5.20℃,the insulation can guarantee the thermal stability of Qinghai-Tibetan railway.Geothermal field of permafrost has influence on applicable range of the insulation and the influence of MAGT varies with the height of embankment.
  • YANG Guo-jing, DING Yong-jian, XIAO Du-ning
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 701-708. https://doi.org/10.7522/j.issn.1000-0240.2005.0105
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    The relationship between forest and water budgets of mountain catchments is the subject either in ecology or hydrology.The eco-hydrological effects of the forest landscape pattern in the Qilian Mountains of the northwest China are evaluated with the cases of the Dayekou River catchment(DYK) and Haichaoba River catchment(HCB) in this paper.Forest map(1:50 000) of 2001 and topographic maps(1:50 000) are used as inputs to produce the landscape maps.Using ArcGIS,the landscape pattern and eco-hydrological effects of the two catchments are analyzed.The results show that the forest of Picea crassifolia growing on the lower land in DYK are the main landscape elements,doing more important work in the eco-hydrologic system,and the shrubs distributed on the higher land in HCB are the main landscape elements and of importance in eco-hydrological process.Taking the total of water intercepted by crown canopy,holding water capacity by shatter and soil as indexes to determine the integrate hydrology adjusting function,based on the observations and the mean annual rainfall records,using ArcGIS,the integrate hydrology adjusting function of the two catchments is calculated.DYK can regulate 36% of the annual rainfall,and HCB can regulate 24% of the annual rainfall.The integrate hydrology adjusting function of DYK is more strong than that of HCB.When the forest coverage rises from 38% to 51% in DYK,the integrate hydrology adjusting function will rise from 36% to 44%.This study shows that the large area of forest can raise the hydrological effect,and different forest landscape pattern will bring on different eco-hydrological effect.
  • WANG Yan-jun, JIANG Tong, SHI Ya-feng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 709-714. https://doi.org/10.7522/j.issn.1000-0240.2005.0106
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    Based on observations of 113 meteorological stations over the upper reaches of the Yangtze River,the changing trends of temperature,precipitation,and consulting evapotranspiration are analyzed from 1961 to 2000.The changing trends of annual runoff at Pingshan and Yichang Stations are detected for the recent 40 years.Significant positive changing trends of temperature are observed,especially in the 1990s in the headstreams and Jinshajiang basin in the upper reaches of Yangtze River.The average temperature in the 1990s is 0.35℃ higher than that between 1961 and 1990.Significant positive changing trends of annual precipitation are found in the whole upper reaches of Yangtze River,especially in the headstreams and Jinshajiang basin.The frequency of extreme precipitation events in summer shows a significant increase,which contributes a large amount to the increment in annual precipitation.While the decrease of intensity of annual extreme precipitation events have much to do with the decrease of annual precipitation in the Chuanjiang basin.The consulting evapotranspiration decreases obviously over the upper reaches of Yangtze River,especially in summer in Chuanjiang basin. Slight increasing trend of annual runoff at Pingshan Station and slight decreasing trend of annual runoff at Yichang Station are revealed.
  • WANG Shun-de, ZHANG Hong, WEI Lin, MAO Wei-yi, ZHANG Jian-gang, WANG Fu-yong, SHEN Yong-ping, WANG Jin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 715-722. https://doi.org/10.7522/j.issn.1000-0240.2005.0107
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    The Tarim Basin is the biggest arid inland basin in China.It is located in Asia European Continent and far away from the sea.The Aksu,Hotan,Yarkant and Kaidu-Konque Rivers are four source rivers of Tarim River drainage.The three tributary river systems(Aksu,Hotan and Yarkant) that contribute flows to the Tarim River join just above the Aler gauging station where the Tarim River begins.From the confluence of its three main contributing tributaries,the Tarim River mainstream extends 1321 km to Taitema Lake.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 2003,annual virgin flow of 258.21×108 m3 from four mountains basins of Aksu,Hotan,Yarkant and Kaidu-Konque Rivers drain into the Tarim Basin,more 20.7% than average annual streamflow,is an abundant hydrological year.The annual total virgin flow of Aksu,Hotan and Yarkant above the Aler gauging station are 221.19×108 m3 from the mountains basins,and of the Kaidu-Konque River from Tianshan Mountains 37.02×108 m3.The total discharge of the four source rivers into Tarim River is 47.66×108 m3 in 2003,which three tributary river systems(Aksu,Hotan and Yarkant) contributes 44.08×108 m3 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 210.55×108 m3,occupy up 81.5% of annual virgin flow from mountains basin.Yarkant is only river no water drain into the mainstream of Tarim Rive.The interzone consumed water of the Tarim River mainstream are estimated to be 20.51×108 m3for the upper course,the largest consumed section of the Tarim River mainstream;16.89×108 m3 for the middle course,and 11.16×108 m3 for the downstream course.Comparing with 2002,Consumed water has a decreasing trend in upper and middle streams course,and increasing in the lower course.The fifth ecological emergency water diversion project was carried out in the lower reaches of Tarim River,transfer water from Bosten Lake to the Taitema Lake during March 3rd to July 11th,2003,total 132 days.The project transfers 3.58×108 m3 flows into the mainstream of the Trim River from the Bosten Lake.Outflow 3.455×108 m3 drains into 300 km upstream of Taitema Lake,from Daxihaizi Reservoir,and join streamflow of Churchen River from Kunlun Mountains,final a 200 km2 water area appeared in Taitema Lake in 2003.
  • ZHUANG Li, CHEN Ya-ning, LI Wei-hong, YUAN Su-fen
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 723-733. https://doi.org/10.7522/j.issn.1000-0240.2005.0108
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    At different sections of the lower reaches of Tarim River,the MDA contents of the main constructive species of the arbor,bush,herbaceous vegetation-Populus euphratica,Tamarix ramosissima and Apocynum venetumas show an increasing tendency and a positive correlation with the water table along with the constant increase of the groundwater depth and the distance from river.Among them,the Tamarix ramosissima MDA contents of almost every section occupy the first place in the three,which proves that under the condition of moisture coercing at lower reaches of Tarim River,the oxidizing degree of the cell membrane fat of Tamarix ramosissima is relatively high and it is coerced heavy by the aridity;SOD activity of them also rises gradually with the decline of the water table and presents a positive correlation with the water table.However,POD activity keeps dropping with the gradual increase of groundwater depth and presents a negative correlation with the water table.These results indicate that the membrane fats of Populus euphratica,Tamarix ramosissima and Apocynum venetumas have a strong oxidation under the condition of serious water stress,which results in a large amount of MDA accumulation,activates the protection enzyme system in the body of Tamarix ramosissima at the same time and improves its ability of fighting drought through strengthening SOD activity.The reason why POD activity declines may be that arid environment causes POD control system in plant cell obtuseness or protein formatting ability drop,or there are many ways of removing H2O2 in plant,the concrete reason awaits to be studied further.The comparison of SOD and POD activity of Populus euphratica,Tamarix ramosissima and Apocynum venetumas under the same water table at the same section in the lower reaches of Tarim River reflects the complement of SOD and POD functions,namely they cooperate with each other while the plant cell defends active oxygen and other peroxide free radicals,which makes plant adapt to the arid environment better.The rational ecological water level and(serious) coercing water level suitable for the plant survival,which are reflected by the MDA content and SOD activity under different water table conditions,are compared and analyzed,and then a preliminary inference is gotten.When the groundwater depth in the lower reaches of Tarim River is over 3.12 meters,the growth of Populus euphratica and Tamarix ramosissima begins to be suppressed promptly,about 6 meters of water table will cause serious coercion to Populus euphratica,and ≥8.83 meters of water table can jeopardize Populus euphratica’s existence.And the serious coercing water table and critical water table of Tamarix ramosissima are about 5 meters and ≥8.83 meters,respectively.By contrast,the coercing water table to which Apocynum venetumas can bear is relatively high: more than 3.12 meters water table will cause serious coercion to its growth and lower than 4.42 meters water table will endanger its survival.
  • CHEN Yong-jin, CHEN Ya-ning, LI Wei-hong, LIU Jia-zhen
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 734-741. https://doi.org/10.7522/j.issn.1000-0240.2005.0109
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    Based on the monitoring data of groundwater chemistry and groundwater level influenced by the intermittent water conveyance in the lower reaches of Tarim River from May 2000 to November 2002,the variation of the groundwater chemistry was studied in this paper.It is found that the groundwater chemistry in the whole lower reaches has changed a lot.The groundwater chemistry at the sections near the Daxihaizi Reservoir was influenced earlier than that beyond it.The varying scope of the total dissolved solid(TDS) and the major ions in groundwater is obvious near the Daxihaizi Reservoir.At Yinsu Section,the range influenced by the water conveyance was continual enlarged,it was about 200 m from the channel during the first water conveyance,about 400 m during the second conveyance,about 700 m during the third conveyance,and about 1000 m during the fourth conveyance.As for the groundwater chemistry in a certain site,TDS and the major ions in groundwater increased at the beginning of the conveyance,then it can be interpreted as follows: at the beginning water brought the salt to channel from the place nearby,when more and more water came,the solute was diluted,so TDS and the major ions in groundwater decreased,and the decreasing process was fast in speed at the beginning,then slowed down.In addition,it is assumed that the water conveyance has not removed any salinity in this region,but diluted it.To reduce the salinity in the groundwater and soil,a series of measures on ecology,engineering and management should be carried out.
  • ZHANG Xiao-you, KANG Er-si, ZHANG Zhi-hui, ZHANG Ji-shi
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 742-746. https://doi.org/10.7522/j.issn.1000-0240.2005.0110
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    The stem sap flow characteristics of 25-year-old Populus euphratica trees and their relation to environmental factors were studied based on the heat diffusion principle and using ICT200TE.It is revealed that: 1) The daily variation of stem sap flow of P. euphratica on clear days in the whole growing season can be described with an evident unimodal curve.The sap flow rates in June,July,August,September and October are 13.39,12.07,12.69 and 5.1 L·d-1,respectively.2) In the night there is a weak rising sap flow,suggesting a presence of root pressure.3) A stepwise regression analysis of the sap flow rate per hour and environmental factors shows that the stem sap flow can be affected by a number of environmental factors,which,in terms of the influential degree, can be arranged in the descending order: air temperature,soil moisture content,relative humidity,total solar radiation,soil temperature and wind velocity.
  • ZHAO Liang-ju, XIAO Hong-lang*, LIU Xiao-hong, LUO Lang, LI Shou-zhong, LU Ming-feng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 747-754. https://doi.org/10.7522/j.issn.1000-0240.2005.0111
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    By analyzing the stable carbon isotope ratios(δ13C) of Caragana korshinskii(CK) and Artemisia ordosica(AO) under different planting regimes and micro-habitats in Shapotou Station,the variations of plant leaf δ13C and effects of climatic factors,such as rainfall,relative humidity and temperature,on plant δ13C were investigated.Results show that the δ13C values of CK were higher significantly than that of AO’s(P=0.003),namely the efficiency of water use of CK was higher than that of AO.During the growth period,the variations of two plant δ13C values varied owing to the difference in species and planting arrangements.The δ13C of mixed planting AO and single planting CK and AO had the same change trend,i.e.,a decreasing trend before May,an increasing trend(and increasing to the maximum) at July,and then followed by a decreasing trend.However,variation of δ13C of mixed CK decreased during the whole growth period.The δ13C of AO and CK increased along with the decrease of soil water content.The δ13C ratios of AO and CK in the introduced plants were lower than those in the water cycle test field.In the water cycle test field,the leaf δ13C ratios of single planting CK were higher than those of mixed planting CK,and the changing order in δ13C between mixed planting AO and mixed planting CK was inversely.The variations between the δ13C ratios and the leaf water content of AO and CK are inverse.The responses of the δ13C monthly change values(Δ13Cm) of AO and CK to climatic factor change with plant species.The Δ13Cm of AO exhibited a negative relationship with monthly precipitation,mean monthly relative humidity and vapor pressure,and a positive relationship with temperature.There were significant relationships between the Δ13Cm and temperature with CK.It is revealed that the growth of CK was strongly sensitive to temperature change,and the growth of AO was dependent on precipitation,relative humidity and vapor pressure to a certain extent.
  • FANG Jing, DING Yong-jian
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 755-760. https://doi.org/10.7522/j.issn.1000-0240.2005.0112
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    Measurement of condensation water was carried out on five different underlying surfaces around an artificial oasis in the arid region of China,from July to October in 2004.In this paper,not only the formation process of condensation is analyzed in detail,but also the main effect factors concerning the amount of condensation water are discussed.The results indicate that hygroscopic condensation is the dominate one in the desert oasis,which begins at 16:00~18:00 and ends at 7:00~8:00.Sand water content is the key factor determining whether condensation occurs,but the process of condensation is controlled chiefly by relative humidity and air temperature.Moreover,the daily range of temperature can also affect the condensation amount partly.In the artificial forest,artificial grassland,plain sand without vegetation,up-dune and inter-dune,the monthly mean condensation water is 5.1 mm,4.0 mm,3.1 mm,1.8 mm and 1.0 mm,respectively.
  • ZHANG Zhi-shan, ZHANG Jing-guang, LIU Li-chao, WANG Xin-ping, LI Xin-rong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 761-766. https://doi.org/10.7522/j.issn.1000-0240.2005.0113
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    From April to October 2004,two shrubs were selected to investigate the penetrable precipitation under canopies,and then to simulate the relationship of them.The results show that precipitation was 110.9 mm in the experimental period.Precipitation event was short and spasmodic;the number of precipitation events was partial distribution,with 50% and 80% of precipitation events were less than 5 mm and 8 mm,respectively.The penetrable precipitations under both plant crowns were significantly less than precipitation(P≤0.01)and different each other(P≤0.05).Because of the higher and bigger canopy,Caragana korshinskii has the intercepted precipitation significantly more than Artemisia ordosica.The results from influence of location on penetrable precipitations were 1/3 no significant,1/3 significant and 1/3 very significant different,respectively.The total penetrable precipitation is 10.7 mm and 3.7 mm for C.korshinskii and A. ordosica during the experimental period,respectively.Multiple regression analysis indicates that the relationship of penetrable precipitation and precipitation and precipitation duration has high level of significance(P<0.0001),but the result by stepwise regression analysis shows that the relationship of penetrable precipitation and precipitation duration is low level of significance(P<0.05).Thus,a linear equation is suggested,which would express the relationship better(P<0.0001).Besides,exponential equation between canopy interception and precipitation can express the relationship well(P<0.05).In theory,when precipitation is infinitely great,the interception will be constant,i.e.,the maximum interception will be 3.5 mm for C.korshinskii and 1.0 mm for A. ordosica.
  • XU Zhong-min, CHENG Guo-dong
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 767-773. https://doi.org/10.7522/j.issn.1000-0240.2005.0114
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    Growing evidence demonstrated that human has dramatically altered the global environment.Identifying the specific forces driving environmental impacts is a hot topic in the field of sustainable development.One key limitation to a precise understanding of anthropogenic impacts is the absence of a set of refined analytic tools.Firstly,the analytic utility of the well-known IPAT identity and its newly advance,including the developed ImPACT identity and STIRPAT model,is assessed.Then the stochastic model in details and illustrated its application are introduced.With STIRPAT,it is easy to determine the population and affluence elasticity of impact,using cross-sectional,time-series data,and the antilog of the residuals in STIRPAT can be interpreted as a specific multiplier of technology on environmental impacts or the eco-efficiency of technology.Secondly,taking China as a case,the anthropogenic driving forces of environmental impacts using the STIRPAT model and cross-sectional data in 1999 is unpacked.The ecological footprint was taken as the index of environmental impacts due to its strength in accounting for impacts wherever they occur geographically and providing a common unit of measurement for comparing diverse types of impacts.A series of index like urbanization rate,economic structure,economic system position and natural location are considered in the empirical model.Among these variables,the social and political variables like economic system position and natural location are coded as dummy variables.The quadratic terms of affluence and urbanization rate are included to examine the environmental Kuznets curve hypothesis.Thirdly,the analysis results show that population has a proportional effect(approximately unit elasticity) on ecological footprint,and affluence monotonically increases the ecological footprint with a relative low degree than population. Natural location appears to affect the ecological footprint,with southern China having considerably lower impact than northern China.At he same time,the technological eco-efficiency of sample provinces was discussed in details.The most important finding in the empirical study was that overall finding don’t support the environmental Kuznets curve hypothesis.Finally we discussed the advantage of using the STIRPAT and analyses the reason why not support the environmental Kuznets curve hypothesis in empirical analysis.Based on the analysis of future environmental impacts using estimation model,we put forward that the social adaptation should be taken as the direction of succeeding research.
  • WANG Xin-hua, XU Zhong-min, LONG Ai-hua
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 2005, 27(5): 774-780. https://doi.org/10.7522/j.issn.1000-0240.2005.0115
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    The concept of water footprint has been developed in order to have an indicator of water use in relation to consumption of people.The water footprint of a country /region is defined as the volume of water needed for the production of the goods and services consumed by the inhabitants of the country/region.Closely linked to the water footprint concept is the concept of virtual water concept.Virtual water is defined as the volume of water required to produce a commodity or service.There are two ways to calculate the water footprint.Firstly,the water footprint of a nation /region can be assessed by taking the use of domestic water resources,subtract the virtual water that flows out the country/region and add the virtual water that flow in the country/region.Secondly,the water footprint can be calculated by multiplying the amount of production of goods and services consumed by the inhabitants of the country/region with the virtual water content of the corresponding products which often expressed in terms of cubic meters of water per ton of the product(=liters/kg),add the amount of domestic living water consumption.In this paper,the concept of water footprint and its calculation are put forward.Then the water footprint is computed by provinces of China in 2000.The result shows that in Northwest China the water footprint is higher than that in South and East China.Qinhai Province has the highest water footprint,935.75 m3·(人·a)-1.Guangxi Region has the least water footprint,466.31 m3·(人·a)-1.The average water footprint of China is 601 m3·(人·a)-1.The structures of water footprint in some typical provinces in China are also analyzed,and some ways to reduce the water footprint are bring forward in order to alleviate water scarcity.