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21.
N2O emissions from regional agricultural lands--A case study of Guizhou Province,southwestern China 总被引：3，自引：0，他引：3
To preliminarily study N2O emissions and the importance of environmental parameters on N2O flux from subtropical agroecosystem in China,N2O flux measurements were made at three cultivated agricultural lands in Guizhou Province,southwestern China.Based on the test and validation of daily N2O flux and its several associated variables between DNDC model and field measurements,DNDC model has been employed to estimate total N2O emissions from entire agricultural lands and its spatial distribution at county scale in Guizhou in 1995,and to assess the contributions of cropping practices on N2O emissions. 相似文献
22.
An Improved Method for Modeling Spatial Distribution of δD in Surface Snow over Antarctic Ice Sheet 总被引：1，自引：1，他引：0
Using the recent compilation of the isotopic composition data of surface snow of Antarctic ice sheet, we proposed an improved interpolation method of δD, which utilizes geographical factors (i.e., latitude and altitude) as the primary predictors and incorporates inverse distance weighting (IDW) technique. The method was applied to a high-resolution digital elevation model (DEM) to produce a grid map of multi-year mean δD values with 1km spatial resolution for Antarctic& The mean absolute deviation between observed and estimated data in the map is about 5.4‰, and the standard deviation is 9‰. The resulting δD pattern resembles well known characteristics such as the depletion of the heavy isotopes with increasing latitude and distance from coast line, but also reveals the complex topographic effects. 相似文献
23.
Yetang Wang Shugui Hou Weijun Sun Jan T. M. Lenaerts Michiel R. van den Broeke J. M. van Wessem 《Climate Dynamics》2015,45(9-10):2885-2899
24.
Yetang Wang Harald Sodemann Shugui Hou Valérie Masson-Delmotte Jean Jouzel Hongxi Pang 《Climate Dynamics》2013,40(3-4):731-742
The spatial and temporal variability of snow accumulation near Dome Argus, Antarctica, is assessed using new snow pit and stake measurement data together with existing snow pit, ice core and automatic weather station records. Snow accumulation rate shows large inter-annual variations, but stable multi-decadal levels over the last seven centuries. Spatial variations in snow accumulation within the space of 50 km of Dome Argus are relatively small, probably thanks to the smooth topography. A comparison of theses accumulation observations with ECMWF reanalyses (ERA-40 and ERA-Interim) suggests ECMWF reanalysis captures the seasonal variations, but underestimates the overall snow accumulation at Dome Argus by ~50 %. The moisture sources for precipitation over Dome Argus are examined by means of a Lagrangian moisture source diagnostic, based on the tracing of specific humidity changes along air parcel trajectories, for the period 2000–2004 using operational ECMWF analysis data. Dome Argus mainly receives moisture from the mid-latitude (46 ± 4°S) South Indian Ocean, with a seasonal latitudinal shift of about 6°. Compared to other central East Antarctic deep ice core sites such as Dome F, Dome C, Vostok, and EPICA Dronning Maud Land, Dome Argus has a more southerly moisture origin, probably due to topographic influences on the moisture transport paths. These results have important implications for the interpretation of future ice cores at Dome Argus. 相似文献
25.
The mobility of Cu2+, Zn2+, Ni2+, and Cd2+ in soils treated with red mud was experimentally studied to explore the feasibility of remediation of smelter-contaminated soils. Red mud samples were collected with the Bayer process (BRM) and confederate process (CRM) in the Aluminous Plant of Guizhou Province. Two farmed soil samples were collected from the Niujiaotang mining area, Guizhou Province, Southwest China. One sample was weakly polluted by fly ash; and the other was polluted severely by waste water from the smelter. For evaluating the potential of remediation, the concentrations of free metal ions and the distributions of metals in the soil were determined. The concentrations of free metal ions were measured by using the Donnan Membrane Technique, and the contributions of soil sorbents to the heavy metals adsorptions were calculated with Equilibrium Calculation of Speciation and Transport (ECOSAT). BRM reduced the concentrations of free metal ions in two kinds of soils, while CRM only favored the decrease of the concentrations of free metal ions in seriously contaminated soils. The experimental data also showed a tendency that the concentrations of free metal ions decreased proportionally with the amount of added red mud, which resulted from the increasing adsorption of heavy metal ions in the form of metal ion hydroxides. 相似文献
26.
Sulfur Isotopic Characteristics of Coal in China and Sulfur Isotopic Fractionation during Coal—burning Process 总被引：5，自引：1，他引：5
The determined results of the sulfur contents and isotopic composition of coal samples from major coal mines in 15 provinces and regions of China show that the coal mined in the north of China is characterized by higher ^34S and lower sulfur content, but that in the south of China has lower ^34S and higher sulfur content.During the coal-burning process in both indrstrial and daily use of coal as fuel the released sulfur dioxide is always enriched in lighter sulfur isotope relative to the corresponding coal;the particles are always enriched in heavier sulfur isotope.The discussion on the environmental geochemical significance of the above-mentioned results also has been made. 相似文献
27.
Based on the most recently avalilable petrochemical data from China‘s Continent and the thickness of the crust,the authors have calculated the contents of carbon,sulfur and phosphorus in the lithosphere of China‘s Continent (including the Sedimentary-metamorphic structural layer,the granite layer and the basalt layer)and their distribution in the major types of rocks.In addition,a discussion is made on the significance of the results in the study of global circulation of carbon,sulfur and phosphorus. 相似文献
28.
The chemical forms of Fe, Mn, Zn, Cu, Cr, Pb and Cd in the Huanghe River sediments have been studied by sequential extraction techniques and the comparison with data from the Rhine River sediments has been made. In the Huanghe River sediments the average contents of metals, without exception, are below their respective contents in average shales and very close to their levels in Ca-poor granites. The major portion of metals is combined with the detrital and moderately reducible phases. Both in the Huanghe River and in the Rhine River sediments the distribution ratios of metals between the moderately reducible and the easily reducible phases are generally more than unity. However, the distribution ratios of Mn, Zn and Cd are obviously lower than those of Fe, Cr, Cu and Pb. As a result of contamination, the ratios of Fe, Cr, Cu and Pb show an apparent increase, but no remarkable ratio variation is observed for Mn, Zn and Cd. Metals in the Huanghe River sediments, especially Cu and Zn, show a tendency to be associated with the organic phase. The effect of carbonate on metal association preference seems to be less important than that in the Rhine River although there is higher content of carbonate in the Huanghe River sediments. Cd has a greater percentage of the exchangeable phase, which is similar to the result from the Rhine River sediments. 相似文献
29.
本文试图介绍发生在非冰期,主要是全新世的突然气候变化研究所取得的进展,包括山地冰川和深海沉积物所记录的全新世突然气候变化,季风和干旱气候突然变化,以及突然气候变化与太阳变化的关系。太阳变化对整个全新世气候变化的影响似乎正愈来愈明晰起来。 相似文献
30.