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排序方式: 共有117条查询结果,搜索用时 15 毫秒
41.
桂林市电子沙盘设计及其功能 总被引:4,自引:1,他引:3
桂林市电子沙盘的开发采用了3S技术、多媒体技术和数字化技术, 它以数字化的地形图为基础数据源, 建立数字高程模型; 以卫星遥感数字图像为三维景观的表层粘模。电子沙盘具有二维平面-三维立体图对照显示,任意调整观察的位置、高度、方位、视角等功能, 并可以按预设的路线在空中模拟飞行观察, 给人亲临其境的感觉。同时, 它具有绘制剖面、求算任意区域地表面积和土石方量(水库库容)等功能, 突破传统沙盘的概念。 相似文献
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Zaihua Liu Chris Groves Daoxian Yuan Joe Meiman Guanghui Jiang Shiyi He Qiang Li 《水文研究》2004,18(13):2423-2437
High‐resolution measurements of rainfall, water level, pH, conductivity, temperature and carbonate chemistry parameters of groundwater at two adjacent locations within the peak cluster karst of the Guilin Karst Experimental Site in Guangxi Province, China, were made with different types of multiparameter sonde. The data were stored using data loggers recording with 2 min or 15 min resolution. Waters from a large, perennial spring represent the exit for the aquifer's conduit flow, and a nearby well measures water in the conduit‐adjacent, fractured media. During flood pulses, the pH of the conduit flow water rises as the conductivity falls. In contrast, and at the same time, the pH of groundwater in the fractures drops, as conductivity rises. As Ca2+ and HCO3? were the dominant (>90%) ions, we developed linear relationships (both r2 > 0·91) between conductivity and those ions, respectively, and in turn calculated variations in the calcite saturation index (SIC) and CO2 partial pressure (P) of water during flood pulses. Results indicate that the P of fracture water during flood periods is higher than that at lower flows, and its SIC is lower. Simultaneously, P of conduit water during the flood period is lower than that at lower flows, and its SIC also is lower. From these results we conclude that at least two key processes are controlling hydrochemical variations during flood periods: (i) dilution by precipitation and (ii) water–rock–gas interactions. To explain hydrochemical variations in the fracture water, the water–rock–gas interactions may be more important. For example, during flood periods, soil gas with high CO2 concentrations dissolves in water and enters the fracture system, the water, which in turn has become more highly undersaturated, dissolves more limestone, and the conductivity increases. Dilution of rainfall is more important in controlling hydrochemical variations of conduit water, because rainfall with higher pH (in this area apparently owing to interaction with limestone dust in the lower atmosphere) and low conductivity travels through the conduit system rapidly. These results illustrate that to understand the hydrochemical variations in karst systems, considering only water–rock interactions is not sufficient, and the variable effects of CO2 on the system should be evaluated. Consideration of water–rock–gas interactions is thus a must in understanding variations in karst hydrochemistry. Copyright © 2004 John Wiley & Sons, Ltd. 相似文献
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Devonian reef complexes were well developed in Western Australia and South China, but no detailed direct comparison has been made between reef building in the two regions. The regions differ in several respects, including tectonic, stratigraphic and palaeoceanographic–palaeogeographic settings, and the reef building styles reflect minor differences in reef builders and reef facies. Similarities and differences between the two reef complexes provide insights into the characteristics of platform margins, reef facies and microbial carbonates of both regions. Here we present a comparison of platform margin types from different stratigraphic positions in the Late Devonian reef complex of the Canning Basin, Western Australia and Middle and Late Devonian margin to marginal slope successions in Guilin, South China. Comparisons are integrated into a review of the reefal stratigraphy of both regions. Reef facies, reef complex architecture, temporal reef builder associations, 2nd order stratigraphy and platform cyclicity in the two regions were generally similar where the successions overlap temporally. However, carbonate deposition began earlier in South China. Carbonate complexes were also more widespread in South China and represent a thicker succession overall. Platforms in the Canning Basin grew directly on Precambrian crystalline basement or early Palaeozoic sedimentary rocks, but in South China, carbonate complexes developed conformably on older Devonian siliciclastic strata. Pre-Frasnian reef facies in South China had more abundant skeletal frameworks than in Canning Basin reefs of equivalent age, and Famennian shoaling margins containing various microbial reefs may have been more common and probably more diverse in South China. However, Late Devonian platform margin types have been documented more completely in the Canning Basin. Deep intra-platform troughs (deep depressions containing non-carbonate pelagic sediments — Nandan-type successions) that developed along syndepositional faults characterize Devonian carbonate platforms in South China, but have no equivalent on the Lennard Shelf, Canning Basin where inter-reef areas were more shallow. The South China platform-to-depression pattern was generally continuous from the Lower to Upper Devonian, indicating that many pre-Devonian tectonic features continued to exercise considerable effect through deposition. Localized, fault-controlled subsidence was an important factor in both regions, but similarities in 2nd order aggradation–progradation cycles suggest that eustasy was also an important control on the larger scale stratigraphic development of both regions. 相似文献
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Water temperature, dissolved oxygen (DO), pH, and specific conductivity (spc) were measured in a time interval of 15 min in
a karst spring and the spring-fed pool with flourishing submerged plants in Guilin, SW China under dry weather for periods
of 2 days. Measurements allowed calculation of calcium and bicarbonate concentrations ([Ca2+] and [HCO3
−]), and thus CO2 partial pressure (
) and saturation index of calcite (SIc). Results show that there were not any diurnal variations in the physico-chemical parameters
of the water for the spring. However, during daytime periods, pool water decreased to far less than the spring water in a few hours, pH and SIc increased to greater than the spring, and [Ca2+] and [HCO3
−] decreased to less than the spring. During nighttime periods, pool water returned to or even increased to greater than the spring, pH and SIc decreased to less than the spring, and [Ca2+] and [HCO3
−] increased to greater than the spring. The decrease in [Ca2+] and [HCO3
−] to less than the spring during daytime periods implies daytime deposition of calcium carbonate, while the increase in [Ca2+] and [HCO3
−] to greater than the spring during nighttime periods implies nighttime dissolution of calcium carbonate. The direction of
the observed changes depended essentially on the illumination, indicating that daytime photosynthetic and nighttime respiratory
activities in the pool aquatic plant ecosystem, which were further evidenced by the increase and decrease in DO during daytime
and nighttime periods respectively, were the main processes involved. The large variations of the components of the carbonate
system imply considerable changes of the capacities of CO2 and O2 in water. The finding has implications for water sampling strategy in slow-flowing karst streams and other similar environments
with stagnant water bodies such as estuaries, lakes, reservoirs, and wetlands, where aquatic plant ecosystem may flourish. 相似文献
47.
桂林喀斯特石山苔藓植物生态分布的初探 总被引:8,自引:0,他引:8
通过以桂林喀斯特石山地区苔藓植物为研究对象进行取样调查,选择植被比较完整的样地进行典型样点取样,共选取样地15处,样点34个,采集鉴定苔藓植物40种,分属19科32属,其中苔类8科8属8种,藓类11科24属32种。以山顶、山腰、山脚和土生、石生、树生以及干湿状态环境因子组合共划分出18种不同的样点环境类型,应用数学生态学等级分划分类方法的组分析技术,以苔藓植物种在某一样点环境中存在与否的二元数据进行样点类型分划和确定临界种; 并通过样点共有种或相异种的分析,探讨不同环境条件下苔藓植物生态分布特点。研究结果表明: ( 1)运用等级分划分类法组分析技术进行桂林喀斯特石山地区苔藓植物生态分布的研究是可行且有效的; ( 2)桂林喀斯特石山地区的苔藓植物分布与湿度状态关系最为密切; ( 3)桂林喀斯特石山地区苔藓植物与环境最佳适应可依次以小凤尾藓( Fissidens bryoides [ L. ] Hedw . )、尖叶提灯藓( Mnium cuspidatumHedw . )和灰羽藓( Thuidium glaucinum Mit t )作为分划特征种。 相似文献
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大学生市场是旅游的一个重要细分市场,具有很大开发潜力。选取桂林中越大学生作为样本,采用问卷调查,运用频数统计、卡方分布等分析,对其旅游行为进行研究。结果显示:(1)旅游消费背景分析中旅游消费期望和旅游信息获得渠道存在差异。(2)旅游购买决策分析中旅游类型、方式、目的地范围、旅游地停留时间存在差异。(3)旅游购后分析中旅游服务要素关注点存在差异。其存在差异原因在于文化、语言、动机和处境的差异,最后在此基础上提出发展大学生旅游市场的4条建议。 相似文献
50.
外源水对岩溶碳汇的影响——以桂林毛村地下河为例 总被引:10,自引:6,他引:4
以桂林毛村地下河为对象,研究了外源水对岩溶碳汇的影响。观测计算结果表明:外源水进入岩溶区后,由于内外源水相互混合,提高了岩溶水的溶蚀能力,以致DIC含量不断升高,其碳酸盐饱和指数也逐渐增加,SIc由不饱和达到饱和,增加了岩溶碳汇的通量。2010年9月至2011年3月仅以位于地下河上游的小龙背的外源水补给量和地下河出口的HCO3-浓度进行计算,岩溶碳汇通量由2.28×105g增加至2.04×106g,增加了近10倍。碳汇通量的增加固然与沿途大气降水、植被及土地利用等可能产生的CO2输入有关,但更与外源水加入形成的混合溶蚀作用有关。因此,在岩溶碳汇通量计算中外源水的影响作用不容忽视。 相似文献