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41.
Variations in magnetostratigraphy, pedostratigraphy, grain size and magnetic susceptibility of the loess deposits near Beijing have been studied at two sections. The sections are about 400 km east of the main loess deposits in China, have a maximum thickness of 100 m and extend back to 1.1 Ma. The sequence consists of 14 loess–palaeosol couplets (S0‐S14), which correlate well with sequences in the Loess Plateau. Susceptibility records from the sites near Beijing are comparable to the Xifeng, Luochuan and Baoji sections located in the middle part of the Loess Plateau; however, the down‐core variations in the grain size in the Upper Lishi Formation exhibit some differences. The median grain size increases by about 25–30 µm from L4 to L2, with the sandy grains (>63 µm) increasing from 10–20 wt% to 40–50 wt% . This implies that the depositional environment of the dust sources in the Beijing loess section is different in some aspects from the Loess Plateau. The Beijing loess may have had a different dust source than the Loess Plateau. Copyright © 2001 John Wiley & Sons, Ltd. 相似文献
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Wu Jianhua Zhao Yu Yu Mengjuan Zou Xiaoxiang Xiong Jiaqi Hu Xiang 《Journal of Geographical Systems》2023,25(2):265-289
Journal of Geographical Systems - Object matching is a key technology for map conflation, data updating, and data quality assessment. This article proposed a new Voronoi diagram-based approach for... 相似文献
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本文将本文作者发展的辐流体动力学方程精细化了,在新的理论公式中,描述物质与辐射场的热力学变量被彻底分开了,这不仅使得理论自身内部更为一致,也给变星脉动理论计算带来方便,本文亦证明了新老理论是相容的。 相似文献
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The longest chronology from New Zealand so faris from Libocedrus bidwillii Hook. f. (i.e.,from AD 1992 back to AD 1140, a span of 853 years). A subset of 11 chronologies was selected from anetwork of 23 sites to reconstruct past temperaturesbased on the similarity of significant responsefunctions. A comparison of climate data overdifferent seasons with these 11 chronologies wascarried out using a bootstrap transfer function. Average late-summer (February–March) temperature wasselected for reconstruction based on independentverification results. The reconstructed temperaturewas then presented for the period back to AD 1720. The chronologies reconstructed years experiencing hotsummers better than cold summers. The power spectrumof the reconstructed temperatures showed periodicitiessimilar to those of the observed temperatures. Reconstructed temperatures were significantlycorrelated with other proxy climate reconstructionsderived from tree rings in New Zealand. However,unlike the other tree ring-based reconstructions, theLibocedrus bidwillii series reconstructed boththe 1950s and 1970s warming periods. The resultsalso compared very favourably with other palaeoclimateevidence. 相似文献
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Fan Zhang Xiong Xiao Lijie Wang Chen Zeng Zhengliang Yu Guanxing Wang Xiaonan Shi 《水文研究》2021,35(8):e14330
Climate factors play critical roles in controlling chemical weathering, while chemically weathered surface material can regulate climate change. To estimate global chemical weathering fluxes and CO2 balance, it is important to identify the characteristics and driving factors of chemical weathering and CO2 consumption on the Tibetan Plateau, especially in glaciated catchments. The analysis of the hydro-geochemical data indicated that silicate weathering in this area was inhibited by low temperatures, while carbonate weathering was promoted by the abundant clastic rocks with fresh surfaces produced by glacial action. Carbonate weathering dominated the riverine solute generation (with a contribution of 58%, 51%, and 43% at the QiangYong Glacier (QYG), the WengGuo Hydrological Station (WGHS), and the lake estuary (LE), respectively). The oxidation of pyrite contributed to 35%, 42%, and 30% of the riverine solutes, while silicate weathering contributed to 5%, 6%, and 26% of the riverine solutes at the QYG, WGHS, and LE, respectively. The alluvial deposit of easily weathering fine silicate minerals, the higher air temperature, plant density, and soil thickness at the downstream LE in comparison to upstream and midstream may lead to longer contact time between pore water and mineral materials, thus enhancing the silicate weathering. Because of the involvement of sulfuric acid produced by the oxidation of pyrite, carbonate weathering in the upstream and midstream did not consume atmospheric CO2, resulting in the high rate of carbonate weathering (73.9 and 75.6 t km−2 yr−1, respectively, in maximum) and potential net release of CO2 (with an upper constraint of 35.6 and 35.2 t km−2 yr−1, respectively) at the QYG and WGHS. The above results indicate the potential of the glaciated area of the Tibetan Plateau with pyrite deposits being a substantial natural carbon source, which deserves further investigation. 相似文献
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Traditionally, some physical details(e.g., magnetic braking, energy transfer, angular momentum loss, etc.) have to be taken into consideration during investigations into the evolution of contact binaries. However, the real evolutionary processes which usually contain several of these physical mechanisms are very complicated as a result of strong interaction between components. To avoid dealing with these factors, a linear relationship is applied to the temperatures of components. It is found that the higher the mass ratio(M_2/M_1) of a contact system, the weaker the deviation from thermal equilibrium.On this basis, a variation trend of fill-out factor(f) changing with mass ratio can be inferred, which is consistent with observations. Moreover, if we stick to this point of view, it should be natural that the number of semi-detached binaries in the predicted broken-contact phase of relaxation oscillations is less than the number in the contact phase. 相似文献
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本文通过对三种矢量数据动态存贮方法的分析比较,并通过实践,找到一种安全可靠并且比较实用的数据动态存贮方式。 相似文献