基于WRF模式的风电场短期风速集成预报方法研究

风能始源于大气的运动,具有很大的随机性和间歇性。风速预测是风电场风功率预测的基础,其准确性具有重要的意义。对于复杂地形条件下,风速的预报一直是各国研究的难点和重点。为了提高风电场短期风速预报的准确性,本研究采用多种边界层参数化方案来集成预报风速,将各单一边界层参数化方案预报的风速及相应的实测风速数据,应用随机森林算法建立集成预报模型,对风电场的短期风速进行集成预报研究。试验结果表明,采用集成预报风速方法,预报的风速误差相比于单一边界层参数化方案预报的风速误差明显减小,对研究区域的风速、风向等气象要素有着较好的模拟效果,能够有效提高风速预报的准确率。     

中小城市实施电子报批的总体方案研究

电子报批是规划管理部门实施信息化办公的一个重要方向和趋势,能够极大地提高规划管理部门办案的规范性、科学性、严密性和高效性。本文提出了中小城市实施电子报批的总体方案,并对系统建设的框架、功能、建设策略、实施模式等关键问题进行了深入地探讨。提出的策略和技术思路对中小城市实施电子报批有较好的指导意义。     

面向实体的空间数据模型

空间数据模型是地理信息系统(GIS) 研究的基础内容.为适应新一代大型GIS的数据量大, 拓扑关系复杂, 数据种类多等特点, 提出了一种新型GIS数据模型---面向地理实体的空间数据模型.它以实体为基本表达对象, 具有较强的空间和语义表现力, 支持语义表达和转换, 便于实现等优点.从空间数据管理, 概念数据模型等方面详细地介绍了该种数据模型.实践表明, 采用该数据模型, 系统对真实世界的实体表现力将大大增强, 数据组织更加合理.      

Absorption of Arsenite on Several Iron （Hydro-）Oxides and Impact from Pre-processing Methods

The absorption reactions of arsenite on Fe （hydro-）oxides are studied. The three absorbent types are Fe（OH）3 gel and two Fe （hydro-）oxides, in which the Fe（OH）3 gel was dried in a microwave oven under vacuum at 80℃. It is found that pH changes from 9.71 to 10.36 in 6 minutes after the Fe （OH）3 gel was mixed with NaAsO2 solution, as the arsenite replaces the OH- in goethite and Fe（OH）3. At the 40th minute after the start of the reaction, pH decreases, which is most probably because that the monodentate surface complex of absorbed arsenite has changed into mononuclear-bidentate complex and released proton. The decline in pH values indicates not the end of the absorption but a change in the reaction type. Temperature and dissolved gas has little effect on these two types of reactions. The total absorption of arsenite increases after the absorbent is irradiated with ultrasound, which also lead to difficulty in separating the solids from solution. The absorption capacity for arsenite of Fe（OH）3 gel dried in a microwave oven under vacuum is 53.18% and 17.22% respectively better than that of Fe （OH）3 gel and gel dried at 80℃. The possible reasons are that the water molecules in the gel vibrates with high frequency under the effect of microwave irradiation, thereby producing higher porosity and improved surface activity.     

应用爆破检验KM-n程序定位精度的研究

采用云南区域数据地震遥测台网近震定位程序“KM—n”,分别测定了2005年1月11～27日进行的“04昆深工程”中18个点位的人工地震参数,以此检验台网近震定位程序“KM—n”的可靠性及台网的地震监测能力。洲定结果表明,对于记录波形初动清晰的人工地震,如果台站位置分布较好,参与定位的台站选择适当,用“KM—n”定位,结果相当准确可靠,误差在2km范围内。     

地质学在旅游资源调查评价与开发中的应用

旅游资源范畴随着旅游产业的发展而在不断扩大,生态旅游和地质科学考察旅游成为旅游的重要发展方向。从分析旅游资源的形成和演化与地质学关系出发,探讨目前旅游资源调查评价与开发中对地质学的应用及其不足,提出以地质遗迹保护为基础建设地质公园是旅游资源开发的一个新发展方向,强调了地质学理论与地质资料在旅游资源保护及可持续利用中的作用。这是提高旅游资源调查与评价水平,开拓旅游新领域,为旅游经济发展服务的最佳切入点。     

Origin of ore-forming fluids in Qinggouzi stibnite deposit,NE China:Constraints from fluid inclusions and H-O-S isotopes

The Qinggouzi stibnite deposit is located in Huashan Town, Jilin Province, in the northeastern margin of North China Craton(NCC). It is controlled by fault structures, hosted within structurally controlled felsic dykes, predominantly surrounded by phyllite, schist and quartzite. This study presents the results of fluid inclusions studies, intending to determine the source of the fluid responsible for ore-formation, hence exploring its metallogenesis. The aqueous biphase inclusions are identified in the stibnite-bearing quartz veins of the deposit. Moreover, aqueous biphase inclusions are further classified into(1) biphase liquid-rich inclusions(1 a) and(2) biphase gas-rich inclusions(1 b) depending upon liquid to gas ratio trapped within the fluid inclusions. Homogenization temperatures for(1 a) and(1 b) range between 114.8℃ to 422℃ and 128.3℃ to 267.5℃, respectively. 1 a and 1 b have salinities of 0.18% to 16.14% NaCl_(eqv) and 1.22% to 12.88% NaCl_(eqv), and density range from 0.43 to 1.02 g/cm~3 and 0.81 to 0.98 g/cm~3, respectively. Sulfur isotopic analysis indicates δ~(34)S_(V-CDT) from 4.4×10~(-3) to 6.5×10~(-3), with an average of 5.2×10~(-3), whereas H isotopes values on δD_(V-SMOW) standard are-100.8×10~(-3) and-107.5×10~(-3), while O isotopes data on δ~(18)O_(V-SMOW) standard range between 20.1×10~(-3) and 20.4×10~(-3). Fluid inclusions study, combining with sulfur and H-O isotopic data reveal that the ore-forming fluids originated from deep source and were subsequently contaminated by meteoric water. Hydrostatic pressure calculation shows that the minimum and maximum pressures are 11.65 and 42.33 MPa, and relevant depths of deposit are estimated to be 1.16 and 4.23 km. Finally, we inferred that Qinggouzi stibnite deposit is a medium-low temperature, low salinity hydrothermal deposit, which is formed by deep source and later contaminated by meteoric water, and is classified as epizonal deposit in terms of orogenic series.     

鹤庆—剑川地区岩溶发育特征及其控制因素

滇中鹤庆—剑川地区碳酸盐岩岩溶极为发育,其空间展布广,以连续纯碳酸盐岩型岩溶层组类型为主,岩溶形态多样,包括溶蚀平原、溶丘谷地、溶丘洼地等类型.滇中鹤庆—剑川岩溶系统具有沿断裂走向展布的显著特点,同时沿断层、褶皱轴部和构造裂隙岩溶发育程度明显较大.结合区域地质构造背景,研究认为鹤庆—剑川地区岩溶系统的发育主要受控于物质...     

基于多源数据的三维城市建模方法

以天津新港三维城市建模为例,介绍了基于二维数据、DEM和3D模型等多源数据的三维城市建模的方法和关键技术。为有效利用现有数据资源快速、准确建立三维城市模型提供了一种经济、灵活、省时、高效的方法。     

湿地水文模型浅析

介绍了湿地系统模型的研究现状。分别阐述湿地水量模型、地表及地下水模型、溶质运移模型、蒸散模型及泥沙运移模型,并对当前湿地综合模型系统进行评述,指出建立湿地模型的意义及存在的问题。