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    30 September 2007, Volume 19 Issue 3 Previous Issue    Next Issue

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    EXPERIMENT OF NEAR SURFACE LAYER PARAMETERS ON DRIFT ICE OVER THE ARCTIC OCEAN
    2007, 19 (3):  163-170. 
    Abstract ( 1568 )   PDF (435KB) ( 1589 )  

    Estimates of near surface layer parameters over 78°N drifting ice in the Arctic Ocean are made using bulk transfer methods with experiment data operated by the Chinese Arctic Scientific Expedition from August 22 to September 3,2003.The results show that the net radiation received by the snow/ice surface is 3.6 W/m2,part transformed into atmosphere through the sensible heat and latent heat, which account for 52% and 31% respectively,and the rest part being lost to deep ice by conductive process.The bulk transfer coefficient of momentum is about 1.16×10-3 near neutral stratification,which is smaller than the results obtained over 75°N drifting ice.However,to compare with the results observed over 75°N drifting ice in the Arctic Ocean in 1999,we can find that the thermodynamic and momentum of interactions between sea and air are significantly different with latitudes,concentration and scale of sea ice.It is very important to consider the effect of sea-air-ice interaction over the Arctic Ocean on the studying climate modeling.

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    A SIMULATION OF THE HEATING EFFECT OF HIGH POWER RADIO WAVE ON THE LOWER POLAR IONOSPHERE
    2007, 19 (3):  171-180. 
    Abstract ( 1818 )   PDF (568KB) ( 1731 )  

    In this paper,the Ohm effect of high power radio wave on the lower polar ionosphere was studied.Based on the heat balance function and continuity function,the modification of ionospheric electron temperature and density by high power radio wave was simulated by using IRI2000 and MSIS as a background.The results show that the external pump can modify the temperature of ionospheric plasma and lead to the rising of the temperature of electron,the increase in the collision frequency and the decrease in the loss rate of electron,and furthermore,induce the modification of electron density.The intensity of modification of temperature and density of electron decreases with the increase of the heating time,that is,it tends to be saturated.In addition,it can be concluded that the characteristic time of electron density is larger than that of electron temperature.Also,the higher the frequency of pump,the weaker the Ohm effect of pump.

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    IDENTIFICATION OF SEABIRD-DROPPING AMENDED SEDIMENTS IN PALAEO-NOTCHES OF NY-LESUND,SVALBARD,ARCTIC
    2007, 19 (3):  181-192. 
    Abstract ( 1833 )   PDF (1234KB) ( 2928 )  

    We collected a 118 cm long and well-preserved sediment profile in palaeo-notches from the first strandflat of Ny-lesund(78°55′N,11°56′E),Svalbard,Arctic,and performed multiple sedimentological analyses,including the lithological characteristics of the sediments,the carbon and nitrogen isotopic compositions and chemical element contents.The results showed that the 70—118 cm layer of the sediments was significantly amended by seabird-dropping.The concentrations of TOC、TN、TS、Se、Sr、CaO、As、Pb、Zn in the sediments are notably enriched,they are significantly correlated with each other,and they have a consistent pattern of change versus depth.These elements are good biomarkers for seabirddropping and population.These results could lay the groundwork for the reconstruction of palaeoclimate and the seabird occupation history between 12 ka B.P.and 4 ka B.P.in Ny-lesund,Svalbard,Arctic.

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    CHARACTERISTICS OF THE REE IN THE BONE TISSUES OF PENGUINS AND SKUAS,ANTARCTICA
    2007, 19 (3):  193-202. 
    Abstract ( 1621 )   PDF (433KB) ( 1732 )  

    Rare earth elements(REE) in the bone tissues of penguins and skuas from Great Wall Station and Zhongshan Station in the Antarctic were determined using an inductively coupled plasma mass spectrometer(ICP-MS).The result shows that the total REE contents in seabirds of Antarctic vary from 0.8μg/g to 3.5μg/g.Enrichment of LREE in the seabirds′ bones suggests that there is some fractionation between LREE and HREE.There are obvious differences in species and regions between penguins and skuas,and the REE contents in the seabirds of Great Wall Station are more than the ones in Zhongshan Station.The diversity also exits in the different bone tissues of the seabirds,and the contents in the leg bone are approximately two times higher than the ones in the wing bone.The REE distribution patterns of the bone tissues in the seabirds show relatively enrichment in LREE,the slope of which shows negative,while HREE keeps stable.There are differences in the REE distribution patterns between penguins and skuas,which relate to the food chain and physiological mechanism rather than the seawater.

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    REFLECTANCE SPECTROSCOPY:A NEW METHOD FOR THE RECONSTRUCTION OF PENGUIN PALAEOECOLOGICAL PROCESS IN ANTARCTIC ORNITHOGENIC SEDIMENTS
    2007, 19 (3):  203-212. 
    Abstract ( 1778 )   PDF (1441KB) ( 1791 )  

    Rapid,non-destructive and simultaneous method such as diffuse reflectance infrared spectroscopy provides potentially useful alternative to time-consuming chemical methods of soil or sediment elemental analysis.To assess the utility of near-infrared reflectance spectroscopy(NIRS) for the determination of elemental concentrations in the ornithogenic sediments and penguin palaeoecological reconstruction,four sediment cores(Y2,Y2-4,Y4,AD3) on the Ardley Island in the maritime Antarctic were analyzed by both chemical and spectroscopic methods.All these sediment cores have been proven to be influenced by penguin droppings in our previous studies.Stepwise multiple linear regression and principal component regression approaches were used to develop calibration models for predicting the concentrations of nine bio-elements including P,Ca,Cu,Zn,Se,Sr,Ba,F and S. The results showed that the correlation coefficients between optimal spectra-predicted and chemically analyzed concentrations of these nine bio-elements were quite high(more than 0.90),and the predicated concentration-versus-depth profiles were very consistent with those from actual chemical analysis.Furthermore,in order to infer the palaeoecological significance of spectra data,principal component analysis(PCA) was used to reconstruct the fluctuation of historical penguin population.Compared with the change pattern of penguin size inferred from the concentration variations of nine bio-elements,they had a very similar trend.Overall,this study demonstrated that using reflectance spectroscopy to infer palaeoecological information recorded in Antarctic ornithogenic sediments is feasible.

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    ABSOLUTE GRAVITY MEASUREMENT BY FG5 GRAVIMETER AT GREAT WALL STATION,ANTARCTICA
    2007, 19 (3):  213-220. 
    Abstract ( 1342 )   PDF (1039KB) ( 1451 )  

    Gravity measurement is of great importance for the height datum in Antarctica.The absolute gravity measurement was carried out at Great Wall Station,Antarctica,using FG5 absolute gravity instrument.The gravity data was processed with earth tide correction,ocean tide correction,polar motion correction and atmospheric correction,and the RMS is within ±3×10-8ms-2.The vertical and horizontal gravity gradients were measured using 2 LaCoaste & Romberg(LCR) gravimeters.The absolute gravity measurement provides fundamental data for the validation and calibration of the satellite gravity projects such as CHAMP,GRACE and GOCE,and for the high accuracy geoid model.

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    RESEARCH PROGRESS IN BIODEGRADATION OF OIL POLLUTION IN POLAR OCEAN
    2007, 19 (3):  221-230. 
    Abstract ( 1496 )   PDF (511KB) ( 2167 )  

    Oil pollution in polar ocean increases with the exploration and utilization of polar area.And oil degradation in polar area is very slow for perennially low temperature there.Biodegradation is a major mechanism of oil degradation from the environment for its economic and effective characters.There are a lot of hydrocarbon-degrading microbes in polar ocean.They play an important role in eliminating oil pollution,and show the potential for bioremediation in low temperature.In this paper,we outline the status of research in areas of oil biodegradation in polar ocean and introduce the hydrocarbon-degrading microbes in polar ocean,factors influencing low temperature biodegradation,biodegradation genes and bioremediation in low temperature.

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    GEOGRAPHICAL DISTRIBUTION OF GENERAL AEROBIC HETEROTROPHIC BACTERIA IN SURFACE SEDIMENTS FROM THE CHUKCHI SEA AND CANADIAN BASIN
    2007, 19 (3):  231-238. 
    Abstract ( 1645 )   PDF (380KB) ( 1340 )  

    This paper determined the abundance of General Aerobic heterotrophic Bacteria(GAB) in surface sediments from the Chukchi Sea and the Canadian Basin by using MPN and discussed their geographical distribution.The result showed that the determination percentages of the GAB were high,even till 100%.The abundance range and averages of GAB for 4℃ and 25℃ were 4.00×102—2.40×106,1.71×106 cell·g-1(wet sample) and 2.40×105—2.40×107,1.10×107 cell·g-1(wet sample) respectively.Not only the abundance range but also the averages of GAB at 25℃ were higher than that at 4℃.The abundance of GAB in sediments showed a tendency of roughly higher in the lower latitudinal area than in the higher latitude.The abundance of GAB increased from east to west in longitude.With the water depth increasing,the abundance of GAB at 4℃ decreased,but it's different at 25℃.It seemed that warmer circumstantial temperature was more suitable for some GAB.

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