白云鄂博矿床成矿构造环境分析

白云鄂博矿床是世界著名的超大型铁铌稀土矿床,但因为其成因和形成时代的证据复杂多样,其成因、形成时代及其形成的大地构造环境均有多种不同认识。笔者等曾对赋矿白云岩成因、成矿时代及赋矿地层白云鄂博群的年代这两个关键问题进行了系统的地质、地球化学研究,获得了一系列关键证据,并对前人资料进行了系统地梳理,论证了白云鄂博矿床赋矿白云岩为一大型微晶丘,而微晶丘是热水沉积形成;确定其成矿时代及白云鄂博群的年代均为早古生代。本文进一步报道了在与白云鄂博群下部相当的腮林忽洞群中发现了宏体化石海绵和腹足类,在白云鄂博群中发现了与腮林忽洞群中相同的振动液化脉和振动液化角砾岩。从而笔者等认为,白云鄂博矿床成矿和白云鄂博群的沉积环境是早古生代被动大陆边缘。     

Oasis evolution and water resource utilization of a typical area in the inland river basin of an arid area: a case study of the Manas River valley

The Manas River valley is a typical inland river basin of an arid area in central Asia, and illustrates oasis evolution and economic development in this region. Based on the historical documents, monitoring data from field surveys, and remote sensing image data, this paper illustrates the oases evolution over the last 2,000 years and analyzes the rapid expansion of the Manas River oasis in the last 60 years. We also examine the relationship between oasis evolution and water resource utilization. We discuss the characteristics and effects of oasis expansion and the proposed adjustment measures for sustainable development of the Manas River valley. The principal objectives of this paper were to analyze the relationship between oasis expansion and water resource utilization over the last 60 years, and to solve the conflict between the continuous expansion of oases and a shortage of water resources to keep development of the Manas River valley sustainable. The results indicate that (1) oasis evolution in the Manas River valley over 2,000 years can be divided into three periods: a period dominated by animal husbandry, a period of semi-farming and semi-grazing, and a farming-dominated period. During the first two periods, the oasis area was limited, water conservancy facilities were poor and water utilization levels were low. In the third period, oasis expansion over the last 60 years shows a large-scale development. (2) The farming-dominated period can be subdivided into four phases according to the scale of water projects and the level of irrigation. Different oasis scales of the four phases show that artificial oasis evolution has a close connection with water resource utilization. (3) The evolution of oases in the Manas River valley raises some environmental problems although it plays an active role in promoting sustainability. Therefore, adjustment measures for the future development of oases could be proposed from the perspective of sustainable development, such as oasis scale control, forbidding reclamation, moderating exploitation of groundwater, and transforming industrial structures.     

VLBI MK5B通道检测软件的设计与实现

针对国际上VLBI专用硬盘记录终端升级到MK5B后,数据记录格式发生了显著变化,设计了能够适应MK5B数据格式的通道检测软件。MK5B通道检测软件主要用于检查硬盘记录器记录数据的可读性以及确认接收机和VLBI终端等观测设备的参数设定。在软件设计过程中,考虑到软件的可维护性及可移植性,采用面向对象的设计方法。通过对两段观测数据的处理表明,MK5B通道检测软件工作稳定,处理结果正确,能够满足工作需要。     

土地利用地图的专题色彩设计

本文基于专题地图的设计原理,为土地利用专题地图提供了颜色设计思路;通过典型案例提出了《第三次全国国土调查工作分类》的具体设计方案,并制作样图验证了该设计方案的合理性。本文对于土地利用专题地图色彩设计的探究可用于第三次全国国土调查相关专题图件的编制,为优化地图设计方案、提高土地利用图的表现力,以及相关行业标准的制定提供参考方案。     

生物炭对土壤理化性质影响的研究进展简

Biochar is an organic material with high carbon content, most aromatic structure and great stability resulting from high temperature thermal conversion (usually < 700 ℃) of organic materials under the completely or in part anoxic condition. Due to its stable chemical properties, biochar has received widely attention as a strategy to reduce greenhouse gas emissions. In addition, biochar shows great potential in soil improvement and environmental pollution remediation, and provides a comprehensive solution for the global climate change, food crisis and ecological pollution remediation. Biochar is a carbon rich material, in association with porous characteristics and high surface area which are favorable to accumulating soil moisture, to increasing the porosity, to reducing density and bulk density, and to promoting the formation of soil aggregation. All the above soil physical improvement can provide a good environment for the growth of plants. Furthermore, biochar is an ideal acidic soil amendment which can improve the pH of acidic soil. It contains nutrient element which can be directly released into soil, and its surface charge and functional groups are conducive to soil nutrient retention, such as the reduced leaching of NH⁺₄ and NO^-₃, PO^3-₄, therefore improve the efficiency of nutrient elements. However, the effect of biochar amendments highly influenced by raw materials and pyrolysis conditions is of inconsistent and sometimes even contrast results can be concluded. In this paper, we summarize the current status and knowledge gaps about the effect of biochar amendments on soil physical and chemical properties and some suggestions are also strengthened. Finally, some possible negative impacts of biochar application and research suggestions are discussed in order to better use of biochar in agriculture.     

Evolution of Topography,Drainage and Biogeography in East Asia during the Cenozoic: Summary of the Third Conference on Earth System Science

Drastic changes in the deep Earth processes and paleoenvironments on the surface occurred in Asia and surrounding regions during the Cenozoic. Driven by India-Asia collision and Pacific plate subduction, the Tibet Plateau region in the west gained its high elevation, whereas lithosphere in east China lost its thickness, and West Pacific margin seas opened, all of which led to the establishment of the present-day topography and drainage pattern. These tectonic-geomorphic processes interplayed with global cooling, re-organization of northern westerlies, Asian monsoon regime and biogeography in this region, which have become the frontier topics in earth sciences.     

Drought–flood variation and its correlation with runoff in three headstreams of Tarim River, Xinjiang, China

The Tarim River lies in the inland area of Northwest China, which has a semiarid or arid climate. Because of relatively scarce precipitation in this area, the main water resource is runoff from a mountainous drainage basin. It is very important to ascertain variations of regular hydrologic and meteorological time series data. Through the use of monthly precipitation and hydrologic data in the three headstream mountain areas of the Tarim River over the past 50 years, this work analyzes the variation of a drought–flood index and annual runoff volume, along with spatio-temporal structures of the index related to runoff at multiple time scales, via non-parametric testing and a wavelet transform method. Wavelet transform can clearly demonstrate many characteristics of the time series, including trend, shift, and major periods. Based on the analysis, the following conclusions can be drawn: (1) the drought–flood indices showed increasing trends for the Aksu and Yarkand rivers, and rose non-significantly for Hotan River. The indices of the three headstreams changed remarkably (p < 0.05) in 1986. The curves of wavelet variance show that significant periods of the indices are 4 and 8 years for Aksu and Hotan rivers, and 8 and 10 years for Yarkand River; (2) runoff of the Aksu and Hotan rivers had significant periods of 6 and 8 years, plus 3 and 9 years for Hotan River; (3) there was significant correlation between the drought–flood indices and annual runoff volume in the three headstreams. The results provide important information toward achieving predictability of flood and drought in Northwest China.     

Geochemical characteristics of oils among real cores in displacement model

Physical simulation experiment on oil displacement is an important approach to understand the mechanism and efficiency of displacement. Physical simulation experiments on water-flooding and chemical flooding in real cores with different lithologies and physical properties, reservoir Rock-Eval, TLC-FID, GC of saturated hydrocarbon fractions and GC-MS of saturated and aromatic hydrocarbon fractions were performed to investigate differences in the geochemistry of residual oils in the cores processed by water-flooding and chemical flooding. After fine sandstone was displaced with the two methods, the preferable replacement efficiency was displayed by the chemical constitutions of residual oils. As to glutenite, water-flooding is less effective, while chemical flooding has excellent performance according to changes in chemical compounds in oils. The results showed that the geochemical characteristics of the reservoir oils and lithology and physical properties of reservoir bed need to be considered in selecting replacement methods. In addition, the geochemical parameters for residual oils slightly changed during water-flooding and chemical flooding, which suggested the water-flooding and chemical flooding could not affect the application of these parameters in geochemistry.     

无人机低空飞行障碍物环境风险评估方法研究——以京津新城为例

无人机应用日益广泛,但随着城市环境建设的不断推进,无人机在城市中安全运行的问题也日益突出,因此无人机低空障碍物环境风险评估成为无人机领域研究的关键问题之一。论文按照不同类型无人机及运行高度将低空空域划分为微型、轻型和小型无人机风险评估区域,在充分考虑无人机自身形状大小、运动约束以及障碍物约束等条件的基础上,提出一种近似点扩张算法,基于障碍物原始边界生成扩张边界,并将其作为低空飞行环境中高风险与低风险之间的风险过渡区。以京津新城为例,分别提取不同风险评估区内的障碍物要素,并基于风险评估技术生成面向微型、轻型和小型无人机多高度层的低空飞行障碍物环境风险地图,按其对无人机威胁程度分为高风险区、高风险过渡区、中风险区和低风险区。实验结果表明:研究区内微型、轻型、小型无人机风险评估区内的风险过渡区分别占10.9%、7.3%、9.0%,该方法可以在考虑无人机与障碍物相互影响的基础上,计算飞行区域内无人机潜在碰撞风险区域,实现对低空障碍物环境风险的科学有效评估,为不同机型的无人机在飞行区域内的可航行性提供科学参考。     

Distribution of heavy metals and nutrients in rainwater in coastal regions between the southern Yellow Sea and East China Sea

Rainwater samples were collected in series in Qianliyan Island (southern Yellow Sea) and Shengsi Archipelago (East China Sea) between May 2000 and May 2002, chemical analysis for pH values,concentrations of heavy metals (Cu, Pb, Zn and Cd) and nutrients (NH4^-, NO3^-, PO43^-, SiO32^-) were performed.Results indicate that concentrations of most of the heavy metals and nutrients in rainwater show clear seasonal variation, i.e. high level in winter and low level in summer. Regionally, concentrations are higher in the southern Yellow Sea than in the East China Sea, but the annual input of heavy metals into oceans by wet deposition is similar in both stations. However, the input of nutrients by wet deposition in the East China Sea is 2-3 times higher than that in the southern Yellow Sea. In individual, Pb and PO4^3- are input to the sea mainly by dry deposition; whereas Cu, Zn, Cd and N compounds are input dominantly by wet deposition, the N/P ratios in the rainwater from two stations are much higher than those in seawater, showing a significant impact of atmospheric wet deposition on marine production and biogeochemical circulation of nutrients in these sea regions.