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81.
含钙铝铁水解聚合产物的矿物学研究Ⅱ:热分解特性 总被引:2,自引:2,他引:0
分别以NaOH和Ca(OH)2作为碱化剂,合成了聚合氯化铝铁(PAFCNa,PAFCCa),比较样聚合氯化铝(PACNa,PACCa)、聚合氯化铁(PFCNa,PFCCa),制成低温干燥样进行热分解检测.热重分析证明,PAFCCa中的含水量高,主要是配位水与结晶水.当n(Al)/n(Fe)>5:5后,PAFCCa的含水量平均为42.3%.按Ca6Al2(SO4)3(OH)12·26H2O分子式计算,钙矾石的结构水(含OH水)含量为43.06%,两者含水量相当接近.TG-DTG热分析结果支持XRD对PAFCCa中存在含Ca3Al2(OH)12柱体的类钙矾石结构体的认定.PAFC-Ca根据其DTG曲线上的125℃和180℃两个脱水速率(肩)峰可以判别其中有无钙矾石结构体,以及相对量的多少. 相似文献
82.
By tracking and monitoring the profile configuration, topography, and hydrodynamic factors of an artificial cobble beach in Tianquan Bay, Xiamen, China over three consecutive years after its completion, we analyzed the evolution of its profile configuration and plane morphology, and its storm response characteristics. The evolution of the profile configuration of the artificial cobble beach in Tianquan Bay can be divided into four stages. The beach was unstable during the initial stage after the beach nourishment the profile configuration changed obviously, and an upper concave composite cobble beach formed gradually, which was characterized by a steep upper part and a gentle lower part. In the second stage, the cobble beach approached dynamic equilibrium with minor changes in the profile configuration. At the third stage the beach was in a high-energy state under the influence of Typhoon Meranti, and the response of the artificial cobble beach differed significantly from that of the low-tide terrace sandy beach. Within a short time, there was net onshore transport of cobbles in the cross-shore direction. The beach face was eroded, the beach berm was accumulated, and the slope of the beach was steepened considerably. In the alongshore direction, there was notable transport of cobbles on the beach from east to west along the shore, and the total volume of the beach decreased by 4.5×103 m~3, which accounted for 50% of the total amount of beach volume lost within three years. The fourth stage was the restoration stage after the typhoon, characterized by a little gentler profile slope and the increase in width and the decrease in height of beach berm. Because of the action of waves and the wave-driven longshore current caused by the specific terrain and landform conditions along the coast(e.g., coastal headlands, near-shore artificial structures, and reefs), the coastline of the artificial cobble beach gradually evolved from being essentially parallel to the artificial coast upon completion to a slightly curved parabolic shape, and three distinct erosion hotspots were formed on the west side of the cape and the artificial drainpipe, and the reefs. Generally, the adoption of cobbles for beach nourishment on this macro-tidal coast beach with severe erosion has yielded excellent stability and adaptability. 相似文献
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The dust deposits in the Yangtze River Basin(YRB) have been widely distributed along the Yangtze River valley. Previous studies mainly concentrated in its provenance of each loess site,however, the differences in provenance of loess among different sites in this area have rarely been studied. Here, the geochemical characteristics of the20 μm fraction in the loess in separate Jiujiang,Xuancheng and Nanjing sites were analyzed. The result shows that the loess in Jiujiang and Nanjing sites, near Yangtze River riverway, share similar geochemical characteristics that may commonly derived from the detrital materials of Yangtze River.However, both sites have significantly different elemental compositions compared with Xuancheng site, which is ~60 km away from the Yangtze River riverway. These sites share different geochemical characteristics with Eastern Qinling Mountains and Xifeng section on the Chinese Loess Plateau, North China. Combining the distribution of the aeolian sand hills and the loess in this area published by previous studies, we suggest that the exposed river valley floodplain caused by weak summer monsoon provided abundant materials to form local dust cells controlled by strong winter monsoon during the glacial periods. Therefore, those local loess deposits should be identified as the "valley-sourced loess".These reveal the inherent connection between the monsoon system and the loess deposits in Yangtze River Basin. 相似文献
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85.
洞穴石笋沉积旋回主要特征的古气候环境研究 总被引:2,自引:1,他引:1
通过对我国南方大型石笋组分、结构构造的观测和董哥洞10号(D10)石笋210件碳、氧同位素组成、20个U系测年数据,以及部分微(痕)量元素的分析对比,概述了石笋沉积旋回性特征、旋回界面类型和相关的气候、环境、地质意义.以组成D10石笋的碳酸盐含碳质、黏土矿物,呈黑灰、灰黄、灰白、灰等色泽匹配、纹层厚及组合、层面呈拱形或平直分别组合或转变、构造类型、碳氧同位素组成及其组合,呈协调平行、不协调同向、不协调反向变化三类型若干亚类等,旋回性特征,确定了19个沉积旋回.根据δ13C平均值为-3.91 ‰PDB、δ18O为-6.97 ‰PDB分别为冷暖气候演变的临界(阀)值,δ13C或δ18O>临界值者的偏重是冷,<临界值的偏轻是热.以δ13C、δ18O组成(表1)和组合变化类型和上述旋回性特征,结合层面构造呈渐变过渡或突变,以及20个同位素年龄数据,初步认定荔波地区352 930~99 410年间沉积的19旋回,是一个较完整的冰期气候演化过程,属我国第四纪冰期系列的第五冰期,10旋回顶180 695年(推算)~15旋回顶129 890年,约5万多年是连续严寒的盛冰期,①、16分别可能是冰期早、晚时段相对温暖的间冰期.期间冷暖变化有5万年级的、10万年级的气候旋回.论证了荔波地区35~10万年间是冰期气候环境,前期17万年寒冷的气候环境,期间35万年、25万年前后更严寒,但生态基本保持正常演变的面貌,中期5万多年为极寒冷的气候环境,生态向适应冷气候环境演化,晚期3万多年为冷暖频繁突(跃)变的恶劣气候,期间生态面貌复杂,正常演替与残存、突变演替并存. 相似文献
86.
GUAN Zhi ZHAO Kai SONG Dong-sheng 《中国地理科学(英文版)》2006,16(1):83-86
1INTRODUCTIONSoil is the basis of human's living. Soil moisture plays asignificant role in studying the matter and energy ex-changes in global hydrology sphere. The evaporation ofsoil moisture has an influence on the water vapor cycle.Meanwhile soil moisture is also one of the firsthandmeasurable parameters in crop yield estimation and wa-ter resources management (JACKSON et al., 1993). Theinfluence of the interaction of land and atmosphere onsoil moisture can bring about anomalous cli… 相似文献
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本文在分析和比较了三维GIS中多种数据结构的基础上,重点讨论了线性八叉树编码原理、线性八叉树数据结构以及线性八叉树的生成、显示与操作,并从数据结构的优缺点着眼,提出将BR 法与线性八叉树相结合的观点;从三维动画技术着眼,提出将原型法、CSG 法与线性八叉树相结合的观点,最后提出一种基于多元表示的三维GIS系统的构想框架 相似文献
90.
用数学形态学变换实现空间分析中的数据处理 总被引:1,自引:0,他引:1
论述了数学形态学的基本算法, 并将这一方法引入空间分析的数据处理中。研究表明,该方法具有一定的可行性, 对于空间分析中一些问题的深入研究具有参考价值 相似文献