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871.
Geopolymer formation and its unique properties 总被引:3,自引:0,他引:3
The characteristic property of naturally-occurring geopolymers is a high content of humic materials that are recognized by the nitrogen function. Through a simulated geopolymerization, biopolymers with non-nitrogen function, such as xanthan gum, were found to have the characteristics of humic acid by means of UV–Vis spectrometry. This fact ascertains that any kind of biopolymer may naturally transform to a geopolymer. A geopolymer is a type of crosslinked long-chain compound, built in three-dimensional structures whose property is immune to microbial degradation. A crosslinked biopolymer was shown to have the same characterization as a geopolymer that has a long life due to its crosslinking capacity and anti-microbial properties. In this study, the formation of petroleum-based geopolymers (e.g., kerogen) was introduced. This study may elucidate the structure of geomacromolecules and the mechanism of their formation, closely related with crosslink reaction between inorganic and organic molecules. This will further change the conventional definition of geopolymer that involves only the inorganic geopolymer. 相似文献
872.
Siew Wei Goh Alan N. Buckley Robert N. Lamb William M. Skinner Allan Pring Haipeng Wang Liang-Jen Fan Ling-Yun Jang Lee-Jene Lai Yaw-wen Yang 《Physics and Chemistry of Minerals》2006,33(2):98-105
X-ray photoelectron spectra have been obtained under the same experimental conditions for synthetic α-NiS and natural β-NiS in order to establish any difference in S electronic environment, and to test the proposition that S core electron binding energies increase measurably with coordination number when the same metal is in different sulfide structures or lattice sites. The Ni and S electronic environments in the two NiS structures have been further probed by near-edge X-ray absorption fine structure (NEXAFS) spectroscopy, and the NEXAFS spectra interpreted by reference to spectra simulated by ab initio calculations. The photoelectron and NEXAFS spectra for freshly prepared surfaces of α-NiS and β-NiS were found to be similar, with only subtle differences in electronic environment evident in the experimental and simulated NEXAFS spectra. The measured and calculated core electron binding energies did not support the previously postulated relationship between S coordination number and electron binding energies. 相似文献
873.
INTRODUCTIONCompositionally ,the term“boninite”refers to alarge variety of pri mary or near-pri mary ( Mg#=0 .60 -0 .85) magmas with a wide variation of CaO/Al2O3(most range from0 .55 to 0 .75) (Crawford etal .,1989) . With regard to its definition as recom-mended bythe I UGS (Deng et al .,1993) and Hickeyand Frey (1982) ,the classification of boninitic rocksis still a matter of petrological debate ( Qiu et al .,2004) .In general ,rock with some typical geochemi-cal features of bon… 相似文献
874.
Ping'an Wang Hiroaki Kaneda Shijiang Ding Xiaowen Zhang Xiangjun Liao Faxian Dong Zhongjian Li Xiaochun Liu Yong Lai 《Resource Geology》2006,56(2):157-166
Abstract. The Baolun quartz vein type Au deposit, is located at the southwestern Hainan Island. It occurs next to a Triassic ilmenite-series/S-type syenogranite complex. A 40 Ar/39 Ar plateau age for muscovite from the master orebody is dated to be 219.4±0.6 Ma, suggesting that the gold deposit genetically related to the granite pluton. In the Baolun mining area, orebodies of auriferous quartz vein and wall rock alteration occur in NNW-striking fracture zones hosted by weakly metamorphosed turbidite of the Lower Silurian age. Eight fracture zones, 400∼1300 m long and 10∼30 m wide, have been identified. The five fracture zones of them form orebodies. The ores are mainly of quartz vein type. More than 20 orebodies in shapes of vein and lens of 195∼751 m in length and 0.20∼7.49 m in thickness are known, and 14 of them occur in the No. 1 vein belt. Silicification, sericitization and pyritization are closely related to the Au mineralization. The ores exhibit commonly 1.54∼29.48 g/t in Au grade, partially >98 g/t. The master orebody is 720 m long and 2.62 m thick in average, with 9.53∼29.27 g/t Au. Gold reserves of more than 70 t have been proven by geological exploration. More than 20 metallic minerals including native gold and sulfides such as pyrite, pyrrhotite, chalcopyrite, and others are identified to be formed in four ore-forming stages: (1) Au-coarse grain quartz stage, (2) Au-fine grained quartz stage, (3) Au-bismuthide-bismuth sulfosalt-sulfide-quartz stage, and (4) calcite-sulfide-quartz stage. The Au mineralization in this deposit occurred mainly in the first three stages. A variety of Bi- and Te-bearing minerals is closely associated with native gold suggesting that the mineralization may take place in a relatively high temperature. 相似文献
875.
Characterizing the dynamic relationship between rainfall and runoff is a highly interesting modeling problem in hydrology. This study develops a deterministic linearized recurrent neural network (denoted as DLRNN) that deals with the system’s nonlinearity by recalibration at each time interval, and relates the weights of DLRNN to unit hydrographs in order to describe the transition of the rainfall–runoff processes. Case studies of 38 events, from 1966 to 1997, are implemented in the Wu-Tu watershed of Taiwan, where the runoff path-lines are short and steep. A comparison between the DLRNN and a feed-forward neural network demonstrates the advantage of DLRNN as a dynamic system model. It is concluded that DLRNN shows superiority in the performance of rainfall–runoff simulations and the ability to recognize transitions in hydrological processes. 相似文献
876.
877.
878.
基于Meta分析的中国森林生态系统生态服务功能价值转移研究 总被引:1,自引:0,他引:1
构建中国森林生态系统生态服务功能价值的数据库和Meta模型,分析价值评估的影响因素,检验模型的有效性。研究表明:①研究方法、生态系统生态服务功能、植被类型、所处植被区域、受益人口数量及集聚程度是影响森林生态系统生态服务功能价值变化的主要影响因素;②有效性检验证明将基于Meta分析的价值转移运用在森林生态系统生态服务功能价值评估上是一种快速且有效的方法;③中国森林生态系统生态服务功能价值呈现东高西低、南高北低的特征,价值随时间推移而增加,涵养水源功能价值最高,提供林果产品功能价值最低。 相似文献
879.
Siqin Tong Jiquan Zhang Yuhai Bao Quan Lai Xiao Lian Na Li Yongbin Bao 《地理学报(英文版)》2018,28(5):595-610
This study analyzed the spatial and temporal variations in the Normalized Difference Vegetation Index (NDVI) on the Mongolian Plateau from 1982–2013 using Global Inventory Modeling and Mapping Studies (GIMMS) NDVI3g data and explored the effects of climate factors and human activities on vegetation. The results indicate that NDVI has slight upward trend in the Mongolian Plateau over the last 32 years. The area in which NDVI increased was much larger than that in which it decreased. Increased NDVI was primarily distributed in the southern part of the plateau, especially in the agro-pastoral ecotone of Inner Mongolia. Improvement in the vegetative cover is predicted for a larger area compared to that in which degradation is predicted based on Hurst exponent analysis. The NDVI-indicated vegetation growth in the Mongolian Plateau is a combined result of climate variations and human activities. Specifically, the precipitation has been the dominant factor and the recent human effort in protecting the ecological environments has left readily detectable imprints in the NDVI data series. 相似文献
880.