晋冀蒙交界地区地壳三维P波速度结构及地震活动性研究

2014年9月晋冀蒙临时地震台网正式运行,为晋冀蒙交界地区的地震研究提供了丰富的资料。结合临时台与固定台记录的P波走时资料,采用双差层析成像方法对该区进行地震重定位和三维P波速度结构联合反演,分析该区3个典型盆地的速度扰动结果,结果表明,地震重定位残差显著降低,震源深度分布更加合理;P波速度浅层基本符合平原地区低速、山区高速的特点,深层则有相反表现,典型盆地P波速度在浅层较为复杂,高低速相间,深层表现为低速;研究时段内忻定盆地和延怀盆地地震活动密集,大同盆地地震活动较弱,低速体及边缘地震活动强度高于高速体及边缘。     

应急流动监测台网在云南巧家M_S 5.0地震中的应用

针对云南巧家M_S5.0地震应急流动测震台站布局规划、台址勘选、仪器设备的架设及组网方式等工作进行归纳总结,并统计分析台站架设后对震区监测能力的提升及余震事件记录的影响,结果发现,流动测震台站的架设提升了台网在震区的监测能力,提高了余震定位精度,使更多余震事件被记录到。     

裂缝暂堵转向重复压裂技术

针对中原油田以往的压裂工艺中单纯采用延伸原有裂缝的常规重复压裂,裂缝所控制的泄油区内的原油采出程度高,但泄油区外的大量剩余油动用程度较低的特点,研制了应用化学暂堵控制剂使流体在地层中发生转向,压裂液进入高应力区或新裂缝层,促使新缝的产生和支撑剂的铺置变化。通过11井次现场应用,累计增油7 162 t。转向压裂技术作为低渗油藏一项重点的配套工艺,更进一步改善了油田的整体开发效果。     

广西平果铝堆积矿分带特征和成矿规律研究

广西平果铝矿区主要分布三种岩溶地貌类型,即岩溶丘陵斜坡型、岩溶峰丛洼地型和岩溶峰林洼地型,它们呈现规律性分布而划分为三个地貌带和对应的堆积型铝土矿带.堆积矿的岩溶地貌分带,是在构造地貌的背景下,由原生铝土矿层的暂时性基准面作用,导致矿区岩溶发育程度变化而形成.通过大量矿化数据的统计分析表明,堆积型铝土矿在化学成分、矿块...     

福山油田保护油气层钻井完井液技术研究

福山油田为典型凝析油气藏,储层孔隙度10%～20%,平均渗透率35?10-3 μm2,属于中孔低渗储层,部分为低孔特低渗储层,且水敏、易塌。通过试验选用了以XZD-Ⅱ为暂堵剂的屏蔽暂堵钻井完井液实施油气层保护,取得了较好的保护效果。     

Simulating streamflow variability and aquatic states in temporary streams using a coupled groundwater-surface water model

Abstract

In order to apply the EU Water Framework Directive for temporary streams, it is important to quantify the space–time development of different aquatic states. We report on research on the development of aquatic states for temporary streams in the Evrotas basin, Greece. The SIMGRO regional hydrological model was used in a GIS framework to generate flow time series for the Evrotas River and all major tributaries. Five flow phases were distinguished: flood conditions, riffles, connected pools, isolated pools and dry bed conditions. Thresholds based on local hydraulic characteristics were identified per stream reach and flow phase, enabling the frequency of flow phases per month and the average frequencies for all streams to be derived. Three historical scenarios within the 20th century, marking periods of major changes in water management, were investigated. Additionally, a climate scenario for the 2050s was analysed. Simulations revealed that low flows are now much lower, mainly because more groundwater is abstracted for irrigation. The consequence is that stretches of the river fall dry during several months, causing the ecological status to deteriorate.

Editor Z.W. Kundzewicz Associate editor X. Chen     

China's Permanent and Temporary Migrants: Differentials and Changes, 1990–2000

A unique feature of migration in China is its two-track system, one consisting of permanent migration and temporary migration. This article examines whether and how hukou reforms and the maturation of migration streams since the 1980s have changed the two-track system. Using data on interprovincial migration from the 1990 and 2000 censuses, our empirical analysis focuses on the differentials between permanent migrants and temporary migrants and their changes over time. We document the size, migration reasons, and selectivity of migrants, and we evaluate the determinants of the dichotomy between permanent migrants and temporary migrants via logistic regression models. Our findings show that between 1990 and 2000 the gaps between interprovincial permanent migrants and temporary migrants did not narrow but in most aspects had widened. There is little evidence that hukou reforms have lowered the barriers to urban citizenship. At the same time, a larger spectrum of the rural population has joined the temporary migration streams. The net result is a persistence of the two-track migration system, where permanent migrants increasingly assume the position of social and economic elites and temporary migrants are the disadvantaged and disenfranchised.     

国家主体功能区战略背景下东北地区城市经济增长的动力与路径——基于城市暂住人口视角

经济、人口、资源与环境的协调发展是新型城市化战略的核心,也是国家主体功能区规划的重要内容。鉴于各类主体功能区在东北地区并存,考察其经济增长与城市化开发路径,可为全国提供较好借鉴。以东北地区城市暂住人口为切入点,探讨了城市暂住人口与经济增长相互影响的作用机制,进而构建暂住人口与经济增长联立方程,并使用东北地区34个地级城市的面板数据进行实证分析,考量以暂住人口吸纳与承载能力为标志的城市化潜力与经济增长的动力。研究表明:在国家主体功能区战略背景下,需充分尊重和考虑东北地区各类开发区域与城市的经济、社会、自然与生态状况,应通过中心城市产业结构调整、生态功能区人口迁出等途径进行集中均衡式的城市化开发,积极加快推进基本公共服务均等化和城市内部基础设施完善。     

Bidirectional stream–groundwater flow in response to ephemeral and intermittent streamflow and groundwater seasonality

It is often assumed that the net groundwater flow direction is towards the channel in headwater streams in humid climates, with magnitudes dependent on flow state. However, studies that characterize stream–groundwater interactions in ephemeral and intermittent streams in humid landscapes remain sparse. Here, we examined seasonally driven stream–groundwater interactions in response to temporary streamflow on the basis of field observations of streamflow and groundwater on an adjacent hillslope. The direction of hydraulic head gradients between the stream and groundwater shifted seasonally. The stream gained water (head gradients were towards the stream) when storage state was high. During this period, streamflow was persistent. The stream lost water to the groundwater system (head gradients were away from the stream) when storage state was low. During this period, streamflow only occurred in response to precipitation events, and head gradients remained predominantly away from the stream during events. This suggested that mechanisms other than deep groundwater contributions produced run‐off when storage was low, such as surface and perched subsurface flowpaths above the water table. Analysis of the annual water balance for the study period showed that the residual between precipitation inputs and streamflow and evapotranspiration outputs, which were attributed to the loss of water to the deeper, regional groundwater system, was similar in magnitude to streamflow. This, coupled with results that showed bidirectionality in stream–groundwater head gradients, indicated that headwaters composed of temporary (e.g., ephemeral and intermittent) streams can be important focal areas for regional groundwater recharge, and both contribute to and receive water, solutes, and materials from the groundwater system.     

Integrating Undergraduate Fieldwork into the Study of Human Mobility

Fieldwork has long been fundamental to human geography; however, increasingly unreceptive institutional environments have led to a decline in fieldwork in undergraduate human geography programs. We argue that mobility research presents an opportunity to reinvigorate the undergraduate field trip in human geography. We report on a second-year field course to Noosa, Australia, that blends new technologies with conventional survey techniques to capture data on a spectrum of human spatial behaviour. Over the course of a single weekend, students collect GPS traces of tourist mobility, survey businesses on the journey to work, collect residential migration histories and trace population dynamics on Noosa beach. Over the three years the course has been running, students have constructed a large repository of data on this Australian mobility hotspot, of which we report highlights. Results from standardised student course evaluations confirm the pedagogical value of these initiatives for human geography undergraduates.