大数据时代的国土资源档案创新管理研究

在大数据时代,以广东省国土资源档案集群服务平台建设为例,以“档案数据大集中、应用系统大集群、档案服务大平台”为总体工作思路,提出了“一个中心,两个集群、三个统一、四位一体”的国土档案管理一揽予解决方案,并对基于大数据的国土资源档案知识服务进行了初步研究,为我国国土资源档案行业在大数据时代信息化建设提供极具实践意义的经验。     

深部坑道围岩压力与变形分析

随着地下空间开发不断向深部发展,出现了用连续介质理论无法解释的现象。以普氏理论为突破口,通过实例分析,从定量的角度出发,找出了普氏压力计算存在的不足,而采用强度理论得出的结果符合实际的物理力学理论。同时也指出,在连续介质理论框架内该强度理论也有其不足,主要在于没有考虑“隐形”区域,暗示为了更精确地描述岩石压力,必须采用新途径。     

Analysis on the sources of mercury in soils in the Chengdu Basin, China

Mercury is a pollutant of concern due to its toxic and bioaccumulative properties. Studies on the distribution and hazard of mercury in the environment are mainly focused on its forms, toxicity and the environment standard, and progresses and results have been achieved. But these studies in the past were concentrated on the scales of laboratory or smaller districts merely, such as a small unit of mineral area, vegetable base, paddy field, lake, etc. Multi-target regional geochemical survey carried out by China Geological Survey from the 1990s to now is a fundamental and commonweal geological survey, large-scale and systematical inquisition and research were conducted in 19 provinces （or municipalities directly under the Central Government） in the eastern overlay region of China, and the purpose is to provide the basic geochemical data for national economic construction, adjustment of industrial and agricultural structures and sustainable social development. Geochemical studies aim at investigating soils in these regions and 52 elements have been tested, producing a great amount of data at the same time. Methods： based on the data from 3061 samples of surface soil and 832 samples of deep soil from the project of multi-purpose geochemical survey in the Chengdu Basin, Sichuan, China, this paper describes the correlation relationship between Hg and other 48 elements and their spatial distribution in surface and deep soils of these areas by applying the method of linear regression and factor analysis.     

超高压变质作用研究现状及问题

本文从超高压变质作用的矿物学、Ｐ－Ｔ－ｔ轨迹和超高压地体抬升、保存机制三个方面总结了近年来超高压变质作用研究所取得的重要进展和存在的问题。超高压变质作用的矿物学研究正在向深入发展，其Ｐ－Ｔ－ｔ轨迹具有三种成因类型。而其超高压地体的抬升、保存机制则是争论的焦点，其中增生楔模式（Ｐｌａｔｔ，１９８７）和连续俯冲─仰冲机制较好地解释了抬升过程，但也存在一些问题需进一步研究。     

CorelDRAW X5中基于VBA实现线渐变的技术研究

主要介绍在CorelDRAWX5中通过VBA的程序开发环境下实现线渐变的方法,通过开发出河流渐变工具,以单线河流渐变为例,解决了通过CorelDRAWX5进行地图制图过程中遇到的单线河流渐变的问题。     

天津海域春夏季节游泳动物的组成特征

根据2014年5月及8月在天津海域进行的底拖网调查资料,对该海域游泳动物组成特征进行了初步研究。结果表明,在该海域共捕获游泳动物36种,平均资源密度为126 297.13个/km~2和1 494.40 kg/km~2。以个体密度计算群落多样性,Shannon-Wiener种类多样性指数H′平均为1.803,Margalef种类丰富度指数d平均为0.592,Pielou种类均匀度指数J平均为0.537。资源密度及物种多样性,8月均优于5月。优势种为口虾蛄,重要种为火枪乌贼、日本、斑、六丝钝尾虾虎鱼。天津近岸海域游泳动物渔业资源呈现出低质化的趋势。     

黄土高原半干旱区异常能量闭合率特征分析

以兰州大学半干旱气候与环境观测站（简称SACOL站）4 a的陆面通量数据为基础,利用普通最小二乘法（OLS）和能量平衡比率（EBR）方法,对能量平衡的异常闭合特征及其与相对垂直湍强（RIw）的关系进行了研究,并进行了能量滞后分析。结果表明,能量过闭合和负闭合现象分别主要发生在白天和夜间,大小遵从正态分布;较大异常闭合产生的原因主要是日出日落时净辐射与地表热通量接近以及降水影响造成湍流通量出现异常大值。一般来说,垂直湍流运动越强,异常闭合越少,闭合度越向1收敛,反之亦然。强湍流或极弱湍流都不利于产生异常闭合,过闭合、负闭合的最适相对垂直湍强RIw约为0.11、0.14。另外,能量支出项的相对滞后也是造成包括负闭合在内的异常闭合的原因之一。剔除湍强较弱的点或将地表热通量G0、感热H、潜热LE相位相对净辐射Rn提前30 min后,异常闭合所占比重减少;月平均EBR法过闭合度降低,OLS法闭合度提高。     

全国分县土地经济系数计算方法及比较

阐述土地经济系数的设置意义和目标,针对全国分县土地经济系数计算,提出并分析比较了统计指标法和分区样点法等思路及其数学处理方法。其中统计指标法中的农业产值消耗法基础数据来源可靠、便利,便于操作,计算结果较好,符合土地经济系数含义要求。     

A new mixing equation for bed material composition in bed form dominant conditions

Vertical mixing beneath the bed surface and its effect on sediment composition has long been underestimated. This paper proposes a mixing equation to illustrate the temporal and spatial variations of bed material composition for bed form dominant rivers. A continuous mass conservation equation for elevation-specific nonuniform bed material composition is initially presented. A vertical mixing equation is finally derived as a diffusion-type partial differential equation with a source term charact...     

Discovering the ancient lakelet of the archeological site of pasargadae in Iran using a multi-layer technique

Pasargadae complex had been the main center of Persian history during the Achaemenian period (560–330 bc), registered as one of the world heritage sites by UNESCO in 2004. This research is an attempt to recognize the natural setting and landscape of Pasargadae during the Achaemenian period, in Iran. The method is based on the application of a multi-layer technique. Collected data by fieldwork, especially in geology, hydrology, and hydrogeology, along with the analysis of aerial data and satellite information provided the baseline information for preparing historic and environmental layers and have made it possible to recognize a natural lakelet in the this area. The results show that the geometry of lakelet together with the ancient river of Pasargadae had been the main elements that formed the character of the site; they were also important in the locations of buildings in the Pasargadae complex.