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151.
Baisha Weng Wuxia Bi Zhixuan Zhao Ting Xu Dengming Yan 《Arabian Journal of Geosciences》2018,11(16):469
Based on the experimental data collected from 2002 to 2010 in Jilin province, we performed multifractal analysis to investigate the spatial variability of soil moisture during 9 years from 2002 to 2010 and about 60 days from April 21 to June 21 in 2010, and analyzed the relationship between soil moisture and precipitation. The results showed that the soil moisture was multifractal. It was intermediate variability in the soil sample. From 2002 to 2010, the spatial variation of soil moisture was charactered by long distance in 2004, 2006, and 2009 and short distance in 2002, 2003, and 2008. The spatial variation of soil moisture was charactered by long distance from April 21 to May 11 and late June. It was charactered by short distance from May 11 to June 21. From April 11 to July 1, 2010, the spatial variation of soil moisture was mainly affected by the spatial variation of precipitation. From 2002 to 2010, the spatial variation of soil moisture was mainly affected by precipitation in 2006, 2009, and 2010. The spatial variation of precipitation had little effect on soil moisture during 2002 to 2005 and 2007 to 2008. This study analyzed the multifractal characteristic of soil moisture from the perspective of water resources divisions, which can provide references for soil water resources evaluation and water resources allocation. 相似文献
152.
潜山走滑转换带在渤海海域发育较为广泛,但其发育特征及控储作用研究薄弱。利用钻井、测井、三维地震等各类资料,对辽东湾北部地区构造转换带发育特征、成因机制及其对潜山规模型储层控制作用进行分析。研究认为,燕山末期左旋走滑背景下,辽东湾北部潜山发育多种类型转换带;根据走滑断层的相互作用以及转换带的形态,可以将辽东湾北部潜山转换带分为单支弯曲型和双支叠覆型两种类型;根据局部应力状态可以进一步细分为单支反“S”型、单支“S”型、双支左旋右阶以及双支左旋左阶转换带4个亚类,其中单支反“S”型和双支左旋右阶型转换带属增压型转换带,单支“S”型和双支左旋左阶型转换带属释压型走滑转换带。增压型走滑转换带提供的压扭性动力破碎作用使得潜山发育大规模裂缝型储集层,是潜山规模型储层发育的关键。 相似文献
153.
LU Lu ZHAO Yuanyi WANG Xiaoliang ZHAO Xitao YANG Zhenjing WANG Chengmin BI Zhiwei LU Wenhui 《《地质学报》英文版》2014,88(5):1565-1578
The platforms on both sides of the Malangou River (a lateral ditch of the Qingshui River that is a tributary of the Yongding River) where Malan Village in Zhaitang Town of Mentougou District of Beijing is located are the place of China's typical section of the Quaternary Malan loess. During the investigation in the eastern suburbs of Beijing City, the authors not only clarified 5 grades of terraces on the Pinggu piedmont plain, but also found a clayey silt section mixed with a small amount of alluvial-diluvial gravel layers at a height of 15-25 m above the river level near a Fishpond in Xinli Village of Nandule Town. Results of the study of grain size of the section document that the loess mostly is silty soil (0.05--0.005 mm), and that the grain size probability cumulative curves of the section are dominated by single-peak, coarse-grained segment I and coarse-grained segment II types, reflecting that its depositional environment is similar to eolian phase. Identification results of heavy minerals from the section show that their contents account for 0.01%-0.11%, averaging 0.04%. There are 24 kinds of heavy minerals, most of which are stable heavy minerals, and the clay minerals mostly are illite, which is consistent with the Malan loess on the Loess Plateau. The chemical composition data reflect that the source area of the loess is relatively arid. The six grade classification of sporopollen in the section further shows the subdivision of the history of alternating warm and humid phases in this geological period. The thermoluminescence dating results range from 21.0 ka to 59.2 ka, convincingly demonstrating that the section indeed consists of Malan loess. The above studies provide a new basis for overall understanding of the distribution of the Malan loess at the northeast margin of the North China Plain and its environment change in the Late Pleistocene. 相似文献
154.
Marshall Geck Xiaoxue Weng Caitlin Bent Taylor Murray Kirsty Wilson 《Climate Policy》2013,13(6):777-784
The reality of the current international order makes it imperative that a just and effective climate regime should balance the historical responsibility of developed countries with the increasing absolute emissions from many developing nations. The key pillars are briefly proposed for a new international climate architecture that envisions replacing the current annex system with two new annexes: Annex α, for countries with high current emissions and historically high emissions, and Annex β, for countries with high current emissions and historically low emissions. Countries in both annexes would implement legally binding targets under this framework. Additionally, this proposal includes alterations and revisions to funding and technology transfer mechanisms to correct for weaknesses and inequities under the current Kyoto architecture. The proposed framework stems from a belief that a top-down, international approach to climate policy remains the most effective for ensuring environmental integrity. Given the slow rate of institutional learning, the reform and improvement of the current system is held as a more efficient course of action than abandoning the progress already achieved. It is argued that the proposed framework could effectively accommodate key equity, environmental integrity, and political feasibility concerns. 相似文献
155.
Pan Ming Huang Shan-Li Wang Yu-Min Tzou Yibin Huang Boqi Weng Shunyao Zhuang Ming Kuang Wang 《Environmental Earth Sciences》2013,68(8):2199-2209
Soil is a vital biological habitat, which is of primary importance in determining and regulating biological activity and biodiversity. Therefore, it is Earth’s most important resource in sustaining both belowground and aboveground biological activities. Biodiversity versus landscape diversity and land use practices in multifunctional landscapes have been addressed. Humans have so manipulated nature that few locations in the world remain without human influence, causing unforeseen changes in ecosystem continuously and biodiversity. Among the environmental compartments, about 90 % of environmental pollutants are bound with soil particles. The soil-bound pollutants may be released to the soil solution through physical, chemical and biological interfacial interactions and pose a threat to biodiversity and ecosystem integrity. These interfacial interactions are especially important in the rhizosphere, where the kinds and concentrations of biomolecules are different from the bulk soil because of intense biological activity. These biomolecules affect biogeochemical processes, soil microbial ecology, nutrient and contaminant dynamics, abiotic and biotic factors, and soil biodiversity through allelopathic interactions. Soil interfacial interactions under different pedogenic processes and anthropogenic activity in relation to belowground biodiversity and the impact on aboveground biodiversity, productivity and integrity should be an important and exciting area of science for years to come. 相似文献
156.
Nick D. Bryan Liam Abrahamsen Nick Evans Peter Warwick Gunnar Buckau Liping Weng Willem H. Van Riemsdijk 《Applied Geochemistry》2012
Some recent developments made during the European Union 6th Framework Integrated Project FUNMIG in the understanding and prediction of behaviour in ternary systems of radionuclides, humic substances and mineral surfaces are described. These developments are placed in the context of the existing literature. The aim is to describe the current understanding of humic substance mediated radionuclide transport as it may be applied to calculations in support of Radiological Performance Assessment. Some improvements in experimental techniques that provide the raw data to calibrate metal ion binding models are explained. The various metal ion binding models that are available are described and contrasted, before the recent development of ternary system models, in particular the Ligand Charge Distribution model that can predict metal ion and humic substance behaviour in ternary systems. The kinetic effects in ternary systems are described along with the models that are used to describe them. Finally, the remaining challenges in making predictions of radionuclide transport for the Radiological Performance Assessment of radioactive waste repositories are discussed. 相似文献
157.
Deng-Hua Yan Jing Feng Chuan-Zhe Li Tian-Ling Qin Bai-Sha Weng Xin Jin 《Natural Hazards》2012,64(1):577-592
This paper focused on the development of a framework for collective water resources management in China to meet the change of drought and flood. Based on the observational data of drought and flood from 1950 to 2009 and the precipitation from 1961 to 2010, using the Standardized Precipitation Index (SPI) method, the evolutionary characteristic of drought and flood was analyzed. The results showed that drought and flood occurred frequently, simultaneous occurrences of drought and flood and the rapid shift between the two were increasing. The framework for collective strategies responding to drought and flood under this ever-changing environment was presented. A series of potential mitigation, prevention, and adaptation strategies were discussed. These included both planning and implementation side strategies. In regard to planning, the strategies for dealing with drought and flood should be shifted from crisis management to collective management, unifying normal and emergency management. Combination risk zoning of drought and flood should be conducted and collective emergency planning should be formulated. Moreover, the regulation capability of water conservancy projects group should be optimized to the highest possible level. In regard to implementation, based on the water resources collective management, rational water allocation for both normal and extreme value processes should be implemented. The water conservancy project groups for the extreme value process should work together, and the flood limit water level of reservoirs should be controlled dynamically. 相似文献
158.
通过对菲律宾南部MD06-3075和婆罗洲东北部MD98-2178两个深海钻孔的孢粉分析,结合氧同位素记录以及西太平洋地区已有的孢粉记录,得到末次冰期研究区域海洋孢粉中的红树林花粉和蕨类孢子含量比间冰期时要低,特别是在末次冰盛期.这可能体现了冰期时海平面较低,湿度较低等环境和气候条件.同时,西太平洋一系列海洋孢粉记录的对比发现,南海南部陆坡地区冰期时的红树林含量仍然较高,巽他陆架等地区冰期时的蕨类孢子含量则表现为明显高值.这些记录的差异可能说明了由于不同地区的地形分布特征不同,在冰期海平面下降时,导致陆架出露的幅度存在明显的差异.如果陆架较宽,则海平面波动会显著改变植被分布范围和孢粉传播距离等,从而对孢粉数据的气候、环境指示意义产生影响.因此,海洋孢粉数据解释时需要结合多种沉积记录指标以及地球物理调查等,提高海平面变化以及相应的沉积环境演化对孢粉搬运沉积的了解程度,增强海洋孢粉中古气候、古环境信息的有效提取. 相似文献
159.
160.
We present a method to unify the calculation of Green’s functions for an electromagnetic (EM) transmitting source embedded in a homogeneous stratified medium. A virtual interface parallel to layer interfaces is introduced through the source location. The potentials for Green’s function are derived by decomposing the partial wave solutions to Helmholtz’s equations into upward and downward within boundaries. The amplitudes of the potentials in each stratum are obtained recursively from the initial amplitudes at the source level. The initial amplitudes are derived by coupling with the transmitting sources and following the discontinuity of the tangential electric and magnetic fields at the source interface. Only the initial terms are related to the transmitting sources and thus need to be modified for different transmitters, whereas the kernel connected with the stratified media stays unchanged. Hence, the present method can be easily applied to EM transmitting sources with little modification. The application of the proposed method to the marine controlled-source electromagnetic method (MCSEM) demonstrates its simplicity and flexibility. 相似文献