The importance of mineral and energy inventories

Based on the results of the Conference on Resource Assessment Techniques of IGCP Project 98 in Loen, Norway, 1976, the importance of mineral and energy inventories is demonstrated by their long-term objectives which aim at the solution of problems of quantitative and qualitative mineral and energy reserve and resource assessments, estimates of the exploration potential, supply analysis, future land-use planning, and national mineral policy. Prior to establishing a mineral and energy inventory it is essential to clearly define both the long-term and short-term objectives, because they control the scope of an inventory and determine the approach to and the method of constructing the data base. Only then can questions be answered as to the kind of data required, the advantages of regional-versus commodity-based inventories, the necessity of computer-processable data files, the availability of a user-oriented data base management system, and the usefulness of conducting a pilot project. Examples are given for simple and complex types of mineral and energy inventories. The “Mineral Deposit Inventory” of the Institute for Geosciences and Natural Resources, Hannover, Federal Republic of Germany, serves mainly as an information and reference system, whereas the mineral inventory of “Project Manitoba” of the Geological Survey of Canada forms the base for reserve and resource assessment as well as land-use planning of that province. For developing and industrialized countries alike, mineral and energy inventories are appropriate tools in planning new exploration activities and decisions on future national mineral policy. Used by the Regional Mineral Resources Development Centers of ESCAP and ECA, the United Nations economic commissions in Asia and Africa, these tools could be of great advantage and mutual benefit to the developing countries of those regions. This paper was presented at the International Geological Correlation Program (IGCP) Project 98: “Standards for Computer Applications in Resource Studies” held at Taita Hills, Kenya, November 8–15, 1977.     

江西某蔬菜基地土壤重金属污染现状

根据表层土、深层土的采样研究资料,获取了江西某蔬菜基地的土壤主要重金属元素基准值,分析了5种重金属元素在该区表层土中的分布、分配及相关特点,分析了元素的迁移特征。对该蔬菜基地的土壤重金属污染现状作了初步评价,并提出了合理调整的相关建议。研究发现,该蔬菜基地表层土(耕作土层)中Cd、Hg、Pb存在明显的积聚现象。局部地段土壤中已超出了农业部颁发的无公害蔬菜产地以及绿色食品产地土壤环境质量标准,成了"不安全生产区"。同时发现区内重金属含量本底值并不高,重金属的污染积蓄主要与人类生产活动有关,可能来源于长期不合理的施肥与喷药。     

"大地测量学基础"课程教学改革的实践

从普通教学型院校测绘教学及测绘市场技术要求出发,针对“大地测量学基础”的课程特点,对教学内容、教学方法及教学手段进行探索与实践,分析多项保证教学质量的改革措施,达到增强教学效果和提高教学质量的目的,论述培养测绘创新人才的诱发、引导、歇留、展现的教学思想,阐述了实际教学全过程的反思,提出了未来教学的有效计划与合理化建议。     

智能化专题地图快速设计制作研究

本文根据专题地图智能化快速设计制作的需求,提出以构建专题地图智能化设计知识库为驱动实现专题地图快速设计制作的模式。在分析其他领域知识和知识库概念的基础上,兼顾该领域的特点,对此模式中知识和知识库的概念重新进行界定。文中以河南省交通图设计为例,基于混合式表示法和此模式下知识库的新特性,构建了专题地图设计知识库的框架体系并进行了阐述。     

球面四元三角网的复杂拓扑关系计算

针对已有球面四元三角网拓扑关系计算方法不能处理带空洞复杂目标的情况,提出了基于公共三角格网来计算球面四元三角网复杂拓扑关系,该方法能准确判断出带空洞复杂目标的拓扑关系,为全球空间分析和应用提供了新的思路。     

增城市地下综合管线信息管理系统设计与实现

增城市地下综合管线信息管理系统是集地下综合管线信息的综合管理和管线数据动态更新于一体,为县域城市规划、建设、管理提供信息资源和管理的技术平台,为政府及各管线权属单位提供了管理决策的科学依据.本文结合增城市地下综合管线信息管理系统的设计理念和研发实践,描述了数据库结构、系统的功能设计和动态更新机制,为探索地下综合管线信息化管理、动态更新维护提供了有效途径.     

基于Web Service的气象预警短信发布系统设计与实现

昆明市气象预警信息发布系统是以提高预警信息及时性和发布效率为出发点,整合了不同种类自动气象站的数据资源,与气象业务平台无缝集成,实时监控数据并生成满足需求的气象预警短信,通过预警号码管理数据库,确定预警信息受众范围,实现了预警短信服务的自动化、标准化、规范化。信息编辑不再需要人工干预,信息发布摒弃了原有的GPRS通信、GSMModem通信、运营商提供短信发布平台等方式,基于Web Service技术直接接入电信短信网关,实现了气象预警信息的高效发布,提高了气象服务的整体质量和效率。     

浅谈通信基站的防雷措施

通过对雷电对通信基站设备的损害分析,提出通信基站相应的防雷措施。     

本科院校交通测量学实训基地建设研究

有效利用教学实训基地能提高学生的职业素养和实践技能。测量学是一门实践性非常强的学科,需要进行实训教学,但目前实训教学基地大多限于高职类院校,本科院校很少进行实训基地项目建设。结合长沙理工大学的交通学科优势和特色,探讨交通类测量学实训基地建设,拓展和完善测量学实践教学的体系,实践证明效果良好。     

Past,present and future vegetation-cloud feedbacks in the Amazon Basin

To begin exploring the underlying mechanisms that couple vegetation to cloud formation processes, we derive the lifting condensation level (LCL) to estimate cumulus cloud base height. Using a fully coupled land–ocean–atmosphere general circulation model (HadCM3LC), we investigate Amazonian forest feedbacks on cloud formation over three geological periods; modern-day (a.d. 1970–1990), the last glacial maximum (LGM; 21 kya), and under a future climate scenario (IS92a; a.d. 2070–2090). Results indicate that for both past and future climate scenarios, LCL is higher relative to modern-day. Statistical analyses indicate that the 800 m increase in LCL during the LGM is related primarily to the drier atmosphere promoted by lower tropical sea surface temperatures. In contrast, the predicted 1,000 m increase in LCL in the future scenario is the result of a large increase in surface temperature and reduced vegetation cover.