25 November 1994, Volume 16 Issue 4
    

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  • Huang Maohuan, Zhou Tao, Jing Xiaoping, Wang Wenti
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 289-300. https://doi.org/10.7522/j.issn.1000-0240.1994.0041
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    A tunnel was excavated in the terminus of the east tributary of Glacier No. 1 at thehadwaters of the Urumqi River. Observations show that ice temperature is close to butslightly lower than the melting point;crystal size is quite large,with the mean diameter reach-ing ten odd milimeters;c-axis orientation mostly appears multi-maximum pattern; thedeformation of the basal layer containing debris contributes immensely to overall motion;and the terminus is an area of radical stress changing, with large strain, significantlongitudinal compression and vertical rising;The principal strain rate is of the order of mag-nitude of 10-1a-1.The elongation,shortening and rotation of the principal axes of strain el-lipses on the wall of the tunnel increase from the back wall towards the tunnel entrance.
  • Xu Xiaozu, Zhang Lixin, Wang Jiacheng
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 301-307. https://doi.org/10.7522/j.issn.1000-0240.1994.0042
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    Assume the Darcy's low is still available for describing moisture movement in frozen soils. The relationship between the frost heave rate and freezing rate, water intake flow rate and temperature gradient for the open system and unidirection treezing of saturated freezing soil is discussed. The laboratory controlled freezing tests under the conditions of the cold plate temperature keeping constant or changing with time are conducted. Results show that the experimental data are in coincidence with the theoritical discussion. And with changing of cooling rate at the cold plate, there are three heave development types of soil freezing appeared: peak type, valley type and successive type. If the cooling rate at the cold plate can be controlled appropriately, then the stable water intake flow, a.i., the total water intake amount changing with time linearly, could be obtained.
  • Yue Hansen
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 308-313. https://doi.org/10.7522/j.issn.1000-0240.1994.0043
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    Restrained by the relation between soil freezing temperature,water content and salt composition,the basic transfer equation of moisture-heat-salt with initial condition and boundary condition comprises the mathematic model for coupled moisture-heat-salt transfer in soil during freezing-thawing processes. The model is required to be amended and improved.
  • Yi Shunmin, Tang Huiming
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 314-319. https://doi.org/10.7522/j.issn.1000-0240.1994.0044
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    Fractal structure features of granulometric composition in frozen soil are studied basedon the fractal theory. The result shows that the fractal dimension of frozen soil is between 2 to3,and its average value is about 2.6.The fractal dimension denotes the evolution propertiesof frozen soil as a selforganizing system. It may be a parameter describing the granulometriccomposition in frozen soil.
  • Cui Guangxin, Li Yi
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 320-326. https://doi.org/10.7522/j.issn.1000-0240.1994.0045
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    This paper demonstrates the experimen ts which are the s tudy on the freezing temperature of wet sand with 4 different water contents under external load of 0-10 MPa with aself-deveoloped freezing point meter.The study shows a law that the freezing temperature ofsaturated and super saturated sand varies with external load.As for the unsaturated sand,itis proved by the experiments that the external load can not influenee the freezing point.
  • Shen Zhongyan, Peng Wanwei, Liu Yongzhi
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 327-332. https://doi.org/10.7522/j.issn.1000-0240.1994.0046
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    The effect of length of specimen on the results in radial splitting test and the correc-tion for computing expression are discussed on the basis of fine test results in this paper.Speciments with seven lengths ranged from 25 to 130 mm are tested under various tem-perature and machine speed(displacement rate controlled by machine).Test results showthat the length of specimen has no substantial effect on detewnined results with radialsplitting method.In the range of slenderness ratio of0.4-2.1, there is little effect on theresults.The strength value determined with radial splitting method is less than that underuniaxial extension,but the ratio between the two is nearly a constant under various tem-perature and machine speed.The results in radial splitting test can be corrected with aconstant K in agreement with the strengths determined under uniaxial extension,so thatthe method is useful in practice.
  • Zhang Yinsheng, Kang Ersi, Liu Chaohai
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 333-341. https://doi.org/10.7522/j.issn.1000-0240.1994.0047
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    The geographic condition make topical features in Urumqi River Valley.Comparingwith low lands,there is a similar seasonal varition of air temperatures in the valley,but opposite trend seasonal varition of relective humidity and more disproporate distribution of pre-cipitation. The laps ratio of air temperature is increased with altitude low than 2400 m a.s.l.and decreased on higher.There is a strong inversion of the air temperature between 1000 to 2400 m a.s.l.from November to next March. The vapour pressure is decreased with altitudebut relective huinidity is increased with altitude excipt few height zone. There are two moreprecipitation zone at 1900 m and 3500 m a.s.l. From 1960s,there is a very little changes ofannal air temperature in the valley but the amount of annal precipitation is much more de-creased.
  • Wang Guangyu, Zeng Qunzhu
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 342-345. https://doi.org/10.7522/j.issn.1000-0240.1994.0048
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    The relationship of 1978(rich snow cover year),1970(poor snow cover vear)andwintersnow covers in three regions of Northern hemisphere to 500 hPa height anomaly and the po-sitions of 100 hPa ridge line of height corresponding to snow covers of 1978, 1970 years areanalysed.The resuIts show 1)500 hPa height anomaly value in 1970 is larger than that in 1978. 2)Winter snow cover of Qinghai-Tibet Plateau has a good relation with 500 hPa heightanomaly in Summer. 3)The position of 100 hPa ridge line in Summer,1978 is more close tosouth than that of 100 hPa ridge line in Summer 1970,the maximum balance reaches 3.37 lat-itudes (120°E,July)。
  • Huang Cuilan, Li Zhongqin
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 346-350. https://doi.org/10.7522/j.issn.1000-0240.1994.0049
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    A determination of major cations in snow and ice cores by employing atomiceabsorption spectrophotometer(AA)is presented.Comparisons between the results and thedata measured using flame optical instrument and ion chromatography(ZC in United States)strongly the instrnment have done a good job to determine the concentrations of indicateNa+,Ca2+,Mg2+ in the snow and ice cores collected in the mountains of western China.Propersampling and sample transportation techniques are suggested to avoid contamination of thesnow and ice samples.
  • Li Gang, Wang Maohai, Huang Maohuan, Wang Wenti
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 351-356. https://doi.org/10.7522/j.issn.1000-0240.1994.0050
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    12 specimens were taken from the base of Glacier No.1 at the headwaters of the UrumqiRiver and machined to be 113 mm in diameter and 200 mm in length. Their debris contentswere 0.01-2.50% by volume,The experiments were treated as uniaxial compresive creepones with constant stress under the conditions of -1±0.3℃ and 0.42 MPa (0.84 MPa for onespecingn).It was found that minimum strain rate appeared at the strain of 1% or so and theparameter of flow law,A,approximatly equals to that ofclean ice. Positive dependence oficecreep on debris content have not been observed.
  • Sun Weizhen
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 357-362. https://doi.org/10.7522/j.issn.1000-0240.1994.0051
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    In this paper an application of PD-1/2 special Automatic control pipette and computerdata processing in the grain-size analysis of glacial deposits is presented.The correctionmethods for estimated error are introdused.It is speculated that this modern analysis methodwill be in good prospect.
  • Li Peiji
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 363-370. https://doi.org/10.7522/j.issn.1000-0240.1994.0052
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    A continuous 500 kyr climate record from vein calcite in Devils Hole,Ncvada shows that the duration of the last four glacial cycles increased from 80 kyr.to 130 kyr.This variationindicates that major climate changes were aperiodic. Broecker(1992)questioned the validityof the Milankovitch theory.He suggested that althouth the date of the end of the penultimateice age(termination 11)was only 17 kyr.earlier than the previously accepted date of 128 kyr.this change is enough to bring the Milankovitch mechanism into serious deubt. Shackleton (1993) refuted the argument.He commented that the discrepancy arises dat-ing of the Devils Hole calcite vein by measuring the growth of 230Th from its parent 234U,because 230Th is produced by decay ofdissolved 234U in the water. Additionally, the value of 140±3 ka was deteimined by interpolation between the closest directly dated subsamples(132 ±3 and 150±3ka)。Imbrie(1993)demonstrated that applying the Devils Hole chronology to ocean cores requires physically implausible changes in sedimentation rate,therefor transfer it to the marinerecord is inappropriate,And the evidence in favour ofmilankovith theory remains strong. Emiliani(1993)suggested that terminations,transitional episodes which extend throughtime,are poor time markers for the correlation of pleistocene section, The maxima(hypsithermals)and especially the minima(bathytherinals)in the isotope curves are muchsharuer and thus afford a more precise correlation. The astronomical parameters can triggeronly the initiation of an ice age,further development of glaciation and deglaciation is drivenby the internal dynamics of the ice-ocean-atmosphere system.The timing of high sea levels over the past 200 kyr.(Gallup et al.,1994)concluded thatfor the last three interglacial and two intervening interstadial rteriods,sea level peaked at orafter peaks in summer insolation in the Northern Hemisphere. This overall patternsupportsthe idea that glacial-interglacial cycles are caused by changes in Earth’s orbital geometry.Crowley suggests that both the Devils Hole and deep-sea chronologies may be correct,with differences between 130 ka and 150 ka years ago reflecting a regionally varying to cli-mate shifts associated with a very extensive glaciation. And extending the vostok ice-core record back to the penultimate glacial period(~140-200 ka ago)yields a new glaciologicaltimescale which is consistent with ocean records.
  • Wang Jianmin, Zhong Wei
    JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY. 1994, 16(4): 371-379. https://doi.org/10.7522/j.issn.1000-0240.1994.0053
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    One of the most dramatic climate change events is the Younger Dryas,a return tonear-glacial conditions during ~10-11 ka BP. that punctuated the last deglaciation,It began and ended with large climatic shifts that took place very abruptly and globally.Possiblemechanisms that created these abrupt climatic shifts are under intense investigation. Many ofhypothesis are summarized in this paper.Although the cause of the Younger Dryas coolingremains an enigma a general consensus seems to be emerging that,the change of oeean current,together with the modification and interaction of oceanic-atmospheric system mayprobably be the key to understanding the such analogoues events of sudden climatic changes。