自我叙事式解读回族宗教活动空间的意义   总被引：4，自引：1，他引：3  

白凯 《地理学报》2012,67(12):1698-1715

基于主位研究视角,以作者自我叙事的方式,对回族宗教活动空间的存在主义意涵进行了主体意向性解读,完整自叙和沉浸思考后作者认为,回族宗教活动空间存在以下特征：① 回族宗教活动空间的核心构成为家、清真寺和坟园;② 家、清真寺和坟园对回族宗教信仰者而言,不是单一的物理空间,而是具有特殊意义的宗教“地方”;③ 说明了回族宗教活动空间具有地方到无地方的转化特征,无地方转换的地方指向是清真寺;④ “接都哇”这一宗教仪式和宗教行为构建了回族宗教活动空间从空间到地方,从地方到无地方转换的桥梁。该分析过程与结论说明了回族宗教活动空间具有从地方的物质宗教空间结构到无地方的精神宗教空间结构的递进转换特征。  相似文献   

一次强天气过程天山地形方案的敏感性试验研究   总被引：1，自引：0，他引：1  

马玉芬  赵玲  赵勇 《中国沙漠》2012,32(4):1127-1134

为定量研究天山山脉地形对新疆强降水天气的影响作用,用WRFV3.1模式对2009年5月24日夜间至26日夜间新疆地区自西向东出现的降水、大风、降温天气过程进行了数值模拟,并通过改变天山山脉的地形高度设计了一组敏感性试验。结果表明:①天山山脉的地形作用是此次强降水天气过程在天山山区形成暴雨的主要原因之一;随着地形的升高,降水分布更不对称,更不均匀,雨带在天山迎风坡一侧的带状分布特征越明显,迎风坡一侧的降水量极值越大;地形的抬升作用对暴雨在山脉迎风坡一侧的降雨量有明显的增幅作用,对其雨带分布也有显著影响\.②天山山脉对这次强降水天气过程中的西南暖湿气流有明显的分流与阻挡作用;天山山脉将西南暖湿气流分为南北两支,使北支的水汽混合比极大值减小,湿区范围增大;使南支的水汽混合比极大值增大,湿区范围增大。③天山山脉的地形抬升作用为“5·25”强降水过程在天山山区发生暴雨天气创造了水汽的垂直上升运动条件,对昆仑山北坡暖湿气流的垂直上升运动也有一定的贡献作用。④天山山脉地形对准噶尔盆地西北部直至天山山脉北侧的气流有明显的阻挡与减缓作用,对三十里风区、百里风区、汗腾格里峰北坡强风带的形成有直接而重要的作用;地形高度越高,产生垂直运动的地形抬升机制越强,地形强迫抬升作用产生的垂直上升运动越剧烈\.⑤天山山脉明显地减轻了寒潮天气过程中南疆塔里木盆地的降温幅度,对准噶尔盆地北部的寒潮降温幅度也有一定的减缓作用,对塔里木盆地的“保温”作用较准噶尔盆地明显。  相似文献   

基于多代理人的零售业空间结构模拟   总被引：2，自引：0，他引：2  

朱玮  王德 《地理学报》2011,66(6):796-804

中心地理论的提出由来已久,但对现实中多种因素复杂作用下的中心地体系进行实证研究并指导规划实践一直难以开展。传统模拟研究方法采用数学线性规划的思路,通过优化目标函数来实现对中心地体系的还原与考察,但复杂程度有限,难以用于实证研究和实践。多代理人技术的出现提供了新的研究思路。本文介绍笔者开发的一个零售业空间结构模拟系统。该系统以多代理人技术为基础,通过模拟商业中心和消费者两类代理人的行为,得出商业中心结构分布。商业中心被分为3 个等级,可以根据经营收入调整空间位置和自身服务等级;消费者以一定的频率产生不同等级的购物需求,并以距离为指标选择商业中心作为出行目的地。模拟过程从产生一定数量的一级商业中心开始,经过循环模拟消费者选择行为和商业中心的位置等级调整,最终达到商业中心等级和空间分布的平衡状态。作为对这个模拟系统的检验,分别对5 种典型的消费者空间分布场景进行模拟,包括：均匀分布、单中心、卫星城、分散组团、带形组团。结果表明这个系统的模拟性能稳定,生成的商业中心结构合理。  相似文献   

青海五龙沟矿区泥岩地层冲洗液研究          下载免费PDF全文

肖冬顺  符文  吴琼  孙荣  黄帆  谭松娥  张莹  方小红 《探矿工程》2019,46(9):45-50

摘要：青海五龙沟矿区内存在大量泥岩地层,其特点为粘土总含量高,易吸水膨胀,地层微裂隙多,导致钻探过程中易出现钻孔缩径、坍塌以及岩心采取率不足等问题,严重影响了矿体规模及经济价值的评价,研究适用于该区的冲洗液意义重大。本文通过正交试验研发了一套适用于该区泥岩地层钻探的水基冲洗液,该冲洗液配方为：5%膨润土+2%纯碱（Na2CO3）+0.05%高粘聚阴离子纤维素（HV-PAC）+0.4%低粘钠羧甲基纤维素（LV-CMC）+2%磺甲基酚醛树脂（SMP-1）+2.5%无荧光防塌润滑剂（FT-342）+0.4%正电胶（MMH）+1%白油。该冲洗液失水量为4 mL,泥岩在清水中的膨胀率为20.26%,而在冲洗液中降到了3.02%,将泥岩制样放到冲洗液中浸泡24 h,泥岩结构保持完整。该冲洗液滤失量低、抑制性强、配制工艺简单,能很好地适用于五龙沟地区泥岩地层的钻探工作。  相似文献   

哈尔滨沙尘沉降物物源敏感粒度组分的提取及来源分析   总被引：1，自引：0，他引：1  

谢远云  梁鹏  孟杰  何葵  臧淑英 《地理与地理信息科学》2009,25(6)

采用粒级-标准偏差算法对哈尔滨2006年3月10日沙尘沉降物进行了物源区敏感粒度组分的提取,获得各来源组分的粒级范围和含量,并进一步分析了不同粒级成因组分的来源.研究认为:1)19.2 μm是哈尔滨2006年沙尘天气颗粒短期悬浮和长期悬浮之界限,而152.4 μm是沙尘颗粒悬浮搬运的粒径上限.2)20 μm作为粉尘物质短期悬浮颗粒与长期悬浮颗粒之界限具有普遍性,而悬浮载荷的粒径上限则与一定的风力条件和地表状况密切相关.3)沙尘沉降物包含4个物源区组分,粒径范围分别为:<1 μm(组分1)、1～19.2 μm(组分2)、19.2～152.4 μm(组分3)和>152.4 μm(组分4).前2个组分属长期悬浮组分,其中组分1代表大气粉尘的本底值;组分2代表非本地源的远距离外源输入,可能与高空气流的搬运有关,包括甘肃和内蒙古在内的半干旱地区为哈尔滨沙尘提供了一定量的粉尘物质;组分3为短期悬浮组分,主要是区域内部沙尘天气产生,松散地表裸土是该组分的重要物源;组分4为跳跃或滚动组分,源于近源物质堆积,是就地起沙.4)哈尔滨2006年沙尘天气外源输入约占63.8%,近源和内源输入占36.2%.松散地表裸土的治理仍是哈尔滨防治沙尘天气的工作重点.  相似文献   

Health, sexuality and place: the different geographies of HIV-positive gay men in Auckland, New Zealand     

Myers J 《New Zealand geographer》2010,66(3):218-227

This paper employs interview narratives alongside participant-led photography and caption writing to examine the different daily geographies of 15 HIV-positive gay men in Auckland, New Zealand. Difference for these men is rooted in both their HIV status and their sexuality, and this difference has implications for their engagement with the world at a range of spatial and temporal scales. Giving voice to such experiences begins to answer calls for geographers to consider more deeply the connections between health, sexuality and place.  相似文献   

鸭绿江河口西岸潮滩沉积对流域人类活动的响应     

石勇  刘治帅  高建华  杨旸  王亚平 《海洋学报(英文版)》2017,36(4):54-63

The response to the catchment changes of the sedimentary environment of the western intertidal flat of Yalu River Estuary was investigated by analyzing the vertical variations of the grain size of sediment cores,along with the hydrologic data and human activities in the catchment.The results demonstrated a stepwise decreasing trend for the variations of both the sediment load and water discharge into the sea,which could be divided into three stages as 1958–1970,1971–1990 and 1991–2009.Reservoir construction and the changes of catchment vegetation coverage turned out to be the two predominant contributors to the changes.There are four periods for the variation of the sensitive components of the sediment cores from 1940 to 2010,i.e.,1940–1950,1951–1980,1981–1990 and 1991–2010.The vertical distribution of grain size in the cores mainly varied with the changes of vegetation coverage in the catchment and reservoir construction from 1960 to 1980,whereas it varied depending on the intensity of water and soil erosion in the catchment from 1980 to 1990.Despite the further reduction of the water and sediment input into the sea from 1990 to 2009,this period was characterized by coarsening trends for the grain size of sediment in the estuarine intertidal flat and correspondingly,the significantly increased silt contents of the sensitive component.  相似文献   

Capturing channelized reservoir connectivity uncertainty with amalgamation curves     

《Marine and Petroleum Geology》2017

During reservoir characterization all the geological uncertainties affecting the quantity and distribution of hydrocarbons should be captured to assess the risks affecting final recovery.In a typical modeling workflow the geological uncertainties are accounted for through the construction of a sufficiently large set of 3-D static models. Out of this set, a few representative models are selected and dynamically simulated so as to correlate the geological characteristics of the reservoir with its dynamic performance and to propagate the uncertainty onto the final recovery factors, yet maintaining the computational run time acceptable. In channelized depositional environments, which are strongly heterogeneous, the selection approach must also account for channel connectivity, which plays a key role in the possibility of efficiently draining the reservoir for a reasonable number of wells.This study can be seen as a step forward in the assessment of the risks associated to the development of channelized reservoirs under the assumption that a way to express the concept of channel connectivity is channel amalgamation. Channel amalgamation is here defined through amalgamation curves which are numerically described using a set of indexes whose combination provide spatial information of channel intersections. These indexes were calculated for a full set of 3-D geological models and used to steer the selection of a representative model sub-set for subsequent fluid flow simulations.The validity of the index-based selection was verified on different sets of synthetic reservoir models through the evaluation of the representativeness of the model sub-set in reproducing the uncertainty of the original dataset. Eventually, the existence of a strong correlation between channel amalgamation and production performance was proved. From a practical perspective, the possibility to include channel amalgamation in the assessment of the geological models can considerably improve the representativeness of the selected models for uncertainty propagation thus reducing significantly the number of geological models to be considered.  相似文献   

新疆乌伦古湖沉积物粒度特征揭示的环境信息     

周建超  吴敬禄  曾海鳌 《沉积学报》2017,35(6):1158-1165

在放射性同位素210Pb、137Cs定年的基础上,通过对沉积物粒度参数的分析,探讨了近200年来乌伦古湖沉积物粒度敏感组分特征及其环境意义。研究表明,乌伦古湖WL孔沉积物以黏土和细粉砂为主,但在1970 AD前后,粒度参数发生了突变,其中>16 μm组分所占含量迅速升高,在约1830~1842 AD及1910 AD前后这两个时期,沉积物的粒度参数也有较显著的变化。对沉积物粒度频率分布曲线的分析表明,在对应时期内,沉积物的搬运介质或搬运动力发生了变化。基于此,首先通过粒径-标准偏差方法提取了粒度中的敏感组分C2（7~25 μm）,进而通过粒度敏感组分与器测气象数据的相关性分析,明确了组分C2含量的环境指示意义。结果表明,组分C2含量的大小与研究区冬、春季温度和冬季降水量大小有关,反映了积雪融水入湖的强度。在约1830~1842 AD、1910 AD前后,组分C2含量偏高,反映入湖水量较大、湖泊水位较高。而20世纪60年代到70年代,沉积物粒度参数的显著变化与流域人类活动的影响有关。  相似文献   

Towards Earth AntineutRino TomograpHy (EARTH)     

R. J. de Meijer  F. D. Smit  F. D. Brooks  R. W. Fearick  H. J. Wörtche  F. Mantovani 《Earth, Moon, and Planets》2006,99(1-4):193-206

The programme Earth AntineutRino TomograpHy (EARTH) proposes to build ten underground facilities each hosting a telescope. Each telescope consists of many detector modules, to map the radiogenic heat sources deep in the interior of the Earth by utilising direction sensitive geoneutrino detection. Recent hypotheses target the core-mantle boundary (CMB) as a major source of natural radionuclides and therefore of radiogenic heat. A typical scale of the processes that take place at the CMB is about 200 km. To observe these processes from the surface requires an angular resolution of about 3°. EARTH aims at creating a high-resolution 3D-map of the radiogenic heat sources in the Earth’s interior. It will thereby contribute to a better understanding of a number of geophysical phenomena observed at the Earth’s surface. This condition requires a completely different approach from the monolithic detector systems as e.g. KamLAND. This paper presents, for such telescopes, the boundary conditions set by physics, the estimated count rates, and the first initial results from Monte-Carlo simulations and laboratory experiments. The Monte-Carlo simulations indicate that the large volume telescope should consist of detector modules each comprising a very large number of detector units, with a cross section of roughly a few square centimetres. The signature of an antineutrino event will be a double pulse event. One pulse arises from the slowing down of the emitted positron, the other from the neutron capture. In laboratory experiments small sized, ¹⁰B-loaded liquid scintillation detectors were investigated as candidates for direction sensitive, low-energy antineutrino detection.  相似文献