共查询到20条相似文献，搜索用时 875 毫秒
1.
Bernard P. Boudreau 《Journal of Paleolimnology》1999,22(3):227-251
This review aims to distill and synthesize the existing information on the use of models to describe and predict the distribution and movement of metals in lacustrine sediments. As such it examines the causes of metal diagenesis, the origin and form of the equations that govern these phenomena, and the predictability or measurability of the parameters that appear in the models. The paper concludes by highlighting some seminal results from modelling studies, including the determination of the factors controlling the formation of surficial Mn-Fe-enriched zone or layers, the substantial contribution possible from metal reduction to organic matter regeneration, the calculation of mixing-corrected metal input histories to lakes, and the prediction of growth rates and morphologies for both deep-sea and lacustrine ferromanganese nodules. 相似文献
2.
Groundwater is the major source of water to the Palestinians. Efficient management of this resource requires a good understanding of its status. This understanding necessitates a characterization of the quality of the utilizable volumes. This paper focuses on the assessment of nitrate concentrations in the aquifers of the West Bank, Palestine. A preliminary statistical analysis is carried out for the spatial and temporal distributions of the nitrate concentrations. GIS is utilized to facilitate the analysis and to efficiently account for the spatiality of nitrate concentrations. The analysis was carried out at different spatial levels and key parameters including soil type, watersheds, depth, population, and rainfall. It is observed that elevated nitrate concentrations in the groundwater greatly coincide with increasing rainfall, particularly in the last few years. Results confirm that the annual mean nitrate concentration in the Western groundwater basin has an increasing trend over the period from 1982 to 2004 indicating its vulnerability to contamination. This result can be attributed to the agricultural activities along with the high groundwater recharge. However, leaking septic and sewer systems are considerably causing nitrate contamination of groundwater in populated areas. Overall, the recommendations call for an immediate intervention to manage the quality problems in the West Bank aquifers. 相似文献
3.
在法国“五月风潮”和后现代主义思潮的影响下,拼装理论应运而生。该理论提出了以根茎思维为基础的动态生成哲学观,批判地揭露了现有研究以网络结构为主,忽视空间拓扑的局限,为人文地理学开辟了新的知识空间。一方面,拼装理论在“空间生产理论”“异托邦”和“第三空间”等空间理论的基础上形成“异质生成空间”,强调属性不同的元素互动的同时,更关注时空不断生成、变化的逻辑;另一方面,拼装理论重构了关系,强调“客体的能动性”和“外部联系”,生成“后关系本体论”,承认所有事物都是通过关系进行拼装的。随着拼装理论在人文地理领域的运用,现有的实证研究主要聚焦于政治拼装与流动性、城市拼装与批判城市化、日常生活拼装与非人的能动性,以及与行动者网络理论、复杂性理论的比较研究。为了阐述拼装理论的内涵,增强理论的应用性,本文以案例的形式详细解析了边界拼装蕴含的拼装逻辑。此外,基于拼装理论为人文地理学注入的过程逻辑与克服人类中心主义的理念,以及该理论特征与中国社会转型期的耦合性,期望国内地理学者能批判地运用拼装理论解释中国情境,以便推动中国人文地理学理论与哲学方法论的多元发展。 相似文献
4.
全球化背景下酒吧的地方性与空间性——以广州为例 总被引：10，自引：0，他引：10
在全球化背景下,以广州代表性酒吧为对象,援引第三空间理论和空间生产理论,采用质性研究方法,从消费地理视角解读酒吧的地方性和空间性,重新诠释地方理论以及人地关系认识论。研究表明,广州环市东酒吧的空间建构包括了一种本土对西方、当下本土对历史本土的再结构化过程。在空间实践-空间想象-再现空间三元一体的维度下,酒吧作为地方具有典型的反身性,酒吧影响着主体行为,行为主体构筑的权力话语也成为酒吧空间的意义构成,涉入酒吧消费空间的建构过程。作为一个具有主体性的消费空间,酒吧具有空间生产、空间消费和空间流动的特质。 相似文献
5.
通过梳理历代文学作品尤其是诗词中的玉门关、阳关、嘉峪关,探析这些地理界标在当时人空间认知中的指代;并确定同期中原与西域间的地理界标;比较界标和界标意象,解读两者之间的关系,探讨界标变动的推动因素。分析发现：① 地理界标缘于疆域的变动和边防经略的调整,其规模、位置等自然之形随着丝绸之路路线变迁而改变;② 中原与西域两大空间的界标与国家疆域时而背离、时而重合;③ 当中原王朝管控能力强时,界标与界标意象重合,反之,界标与意象出现背离。借助文学作品来阐释它们的变迁历程,是深入开展边疆史地研究的一次尝试,为历史地理学研究提供新的视角。 相似文献
6.
独龙江流域地貌 总被引：6，自引：0，他引：6
李先之 《云南地理环境研究》1996,8(1):59-72
文章首先概述独龙江流域的地貌基本形态结构，分析现代地貌作用的外营力，讨论地质构造和地表物质对研究区地貌形成的作用和影响。作者着重根据现代冰川分布及其特征、古冰川遗迹、冰缘地貌类型和古冰缘地貌遗迹，研究独龙江流域全新世以来的构造抬升和气候演变。最后分析研究区坡地形成过程，河流地貌的发展与演变，阐述独龙江流域的地貌发育史。总之，文章坚持将今及古的观点，反对泛冰川和泛构造的解释 相似文献
7.
利用2011南极夏季在普里兹湾获取的海水样,检测了Chla、磷酸盐、硅酸盐、硝酸盐和铵盐的含量。结果表明,普里兹湾表层海水中Chla的含量普遍具有冰架边缘>陆架区>陆坡及深海区的分布特征,海冰的消融及水体的稳定性是影响表层海水Chla分布的主要原因。Chla含量的垂直分布与光照条件相关,具有上层水体含量高,随着深度逐渐降低的分布特征。磷酸盐、硅酸盐和硝酸盐的水平及垂直分布特征都与Chla的分布格局相反。表层海水中铵盐的分布特征与磷酸盐等主要营养盐的分布格局相反,冰架边缘、陆架区铵盐的垂直分布特征与陆坡及深海区不同,在冰架边缘和陆架区有机质降解过程主导着水柱中铵盐的浓度,而浮游植物吸收作用与有机质降解过程之间的平衡控制着陆坡及深海区铵盐的垂直分布。根据Chla与营养盐的浓度及分布特征,结合温度、盐度、溶解氧等水文要素,分析探讨了Chla深层最大值现象（DCM）的成因及67.5°S以南表层海水中铵盐对硝酸盐吸收的抑制作用。 相似文献
8.
Effects of tectonics and lithology on long profiles of 16 rivers of the southern Central Massif border between the Aude and the Orb (France) 总被引：1，自引：1，他引：0
The analysis of longitudinal profiles of river channels and terraces in the southern Central Massif border, between the Aude and the Orb, allows the detection of anomalies caused by lithology and/or tectonic distortions. The rivers which have abnormally high slope and non-lithological knickzones indicate the main uplifted zones: the Montagne Noire and the Saint-Chinian ridge. A geomorphological and sedimentological analysis of detrital deposits was carried out as a basis for correlating the different formations, reconstructing the palaeodrainage and finding the main uplift and fluvial incision stages. During the Miocene, uplift remains limited as it is shown by the correlative fine deposits in the Languedocian piedmont. The Messinian incision (5.7–5.3 Ma) does not cross the Saint-Chinian ridge. On the other hand, fluvial incision becomes widespread in the Montagne Noire during the Upper Pliocene (3.4–2 Ma) when coarse deposits overlie either the Pliocene clay in the Orb palaeovalley or the Messinian conglomerates at the Cesse outlet. An Upper Pliocene uplift of the Montagne Noire and of the Saint-Chinian ridge is the cause of this incision and also of the diversion of the Cesse towards the Aude. Where the uplift rate was higher than incision rate, knickzones have developed like in the Avant-Monts south-side. The knickzones of lithological origin maintain a strong vertical stability during all the river incision stages. On the other hand, those of tectonic origin or base level lowering record upstream migration and their rate of retreat is controlled by the river discharge. As incision occurs only during the cold/temperate transition periods during the Quaternary, upward erosion slowly migrates (15 km since the Upper Pliocene, on the Orb) and so does not reach the riverheads. 相似文献
9.
风尘是地球表层系统的重要组成部分,广泛参与地球系统中不同时空尺度的物理、化学和生物过程,对全球气候和生态环境产生重要的影响。中国北方地区发育了世界最广、最厚的风尘沉积,记录了至少22 Ma以来东亚季风演化和亚洲内陆干旱化历史。半个多世纪以来对风尘沉积的气候记录和黄土高原的成因进行了大量研究并取得了丰硕成果,然而对黄土高原风尘物质沉积过程的认识还存在很多问题。例如,近年来基于物源示踪研究对传统的风尘搬运过程提出了新认识,认为虽然黄土主体是风成的,但以前忽略了河流对于碎屑物质的搬运贡献。我们在前人研究基础上从沉积学角度分析风尘沉积过程,发现青藏高原两期抬升与区域构造运动对粉尘沉积起着不亚于气候变化的重要控制作用;同时从沉积-侵蚀和地貌发育过程探讨风力与流水这两种最常见的外动力方式在黄土沉积和黄土高原发育过程中所起的作用,认为风尘的沉积和黄土高原的形成是侵蚀与搬运沉积作用的长期动态平衡过程,风力和流水在其中所起的作用都不是单一不变的,在不同时期和不同区域有可能会同时充当建设者和破坏者的角色。 相似文献
10.
地缘政治理论的提出和发展深刻烙印了地图的影响。在地缘政治发展史中,不同地图投影既服务于各思想家的理论提出,也深入到各思想家在不同时期对自身理论的动态修正。地图投影到底是如何参与到地缘政治理论构建过程中的?本文在既有地缘政治地图研究的基础上,从空间性和文本性两大地图基本属性出发,通过阐释并沟通地图的空间分析与话语分析功能,探讨地图投影与地缘政治理论构建间的关系。一方面,地图投影变形抽象后的心象地图框架为构建地缘政治理论提供了空间依托;另一方面,地图投影通过地图变形在复杂情境中聚集了丰富的文本性含义。在地图投影各层次文本性的互文（互补性叙事）下,新的地图话语得以产生并渗透进心象地图,具象式推动了地缘政治理论核心概念的生成和逻辑关系的构建。综合考虑麦金德的地图观影响,本文对麦金德“心脏地带”地缘政治思想变迁各阶段（1904年、1919年、1943年）地图投影透视的分析验证了该关系框架的解释力。这启示该分析框架在其他地缘政治理论研究中的潜在适用性,更期待在百年变局和复兴全局等交织下的复杂情境中,基于地图投影创新互文下的中国地缘政治理论构建。 相似文献
11.
Arkadiusz Derkowski Jan
rodo&#x; Magdalena Goryl Leszek Marynowski Marek Szczerba Stanis&#x;aw Mazur 《Basin Research》2021,33(1):570-593
The diagenetic history of the Ediacaran sedimentary rocks in the East European Craton (EEC) over the area extending from Arkhangelsk (Russia) in the north to Podolia (Ukraine) in the south was revealed by means of the XRD characterization and K–Ar dating of clay fractions, mudstone porosity measurements and organic geochemistry investigations. Mudstone porosity measurements produced direct evidence of shallow maximum burial of the Ediacaran sediments on the craton (Russia, Lithuania, Belarus, Volyn), not exceeding 1.5 km, and much deeper burial at the cratonic margin, in Podolia and Poland. In general, illitization of smectite and biomarker indices indicates more advanced diagenesis at the cratonic margin. K–Ar dating of authigenic illite–smectite and aluminoceladonite revealed the Palaeozoic age of mineral diagenesis (ca. 450–300 Ma) both on the craton and its margin, with older ages generally observed in the north. When the maximum palaeotemperatures were evaluated from illite–smectite and biomarkers, based on the calibrations from the conventional burial diagenetic sections, a major mismatch was detected for the cratonic area: 100°C–130°C from illite––smectite and tens of oC lower from the lipid biomarkers. This diagenetic pattern was interpreted as the result of short‐lasting (in ky scale) pulses of potassium‐bearing hot fluids migrating from the Caledonian and Variscan orogens deep in the craton interior, effectively promoting illitization in porous rocks without altering the organic matter. Analogous short pulses of fluids were responsible for numerous diagenetic phenomena, including Mississippi Valley‐Type ore deposits, in the American Midwest, in front of the Appalachians. K–Ar dating indicates that the entire Proterozoic sedimentary cover of the Great Unconformity on the EEC remained untouched by measureable post‐sedimentary changes until the early Palaeozoic, thus for over 1000 My, which is an unprecedented finding. 相似文献
12.
The Holocene history of West Basin Lake,Victoria, Australia; chemical changes based on fossil biota and sediment mineralogy 总被引：4，自引：0，他引：4
Peter A. Gell Philip A. Barker Patrick De Deckker William M. Last Ljubica Jelicic 《Journal of Paleolimnology》1994,12(3):235-258
Analyses of diatoms, ostracods, pollen and sediment mineralogy from a 524 cm core from a stratified, hypersaline crater lake, West Basin, Victoria, has revealed clear shifts in the lake's water balance and chemistry and the region's climate over the last 10 000 years. Diatom and ostracod analyses reveal lake water salinity changes which are consistent with the conditions suitable for the precipitation of the carbonate and other minerals identified using x-ray diffraction analysis. The fluctuations in lake water balance deduced from diatom and ostracod inferred lake salinity suggest that the lake began to fill at the beginning of the Holocene and was saline and shallow. Toward the mid-Holocene the water levels rose and yet the lake remained largely saline. The late Holocene is marked by a return to more shallow but fluctuating, water conditions. Through the whole period, the regional dryland vegetation was dominated by open sclerophyll woodland. Both the lacustrine and regional environments interpreted here are consistent with those from Holocene records elsewhere in the region.This is the fourth in a series of papers published in this issue on the paleolimnology of arid regions. These papers were presented at the Sixth International Palaeolimnology Symposium held 19–21 April, 1993 at the Australian National University, Canberra, Australia. Dr A. R. Chivas served as guest editor for these papers. 相似文献
13.
Probabilistic landslide hazard assessment at the basin scale 总被引：32，自引：9，他引：32
Fausto Guzzetti Paola Reichenbach Mauro Cardinali Mirco Galli Francesca Ardizzone 《Geomorphology》2005,72(1-4):272-299
We propose a probabilistic model to determine landslide hazard at the basin scale. The model predicts where landslides will occur, how frequently they will occur, and how large they will be. We test the model in the Staffora River basin, in the northern Apennines, Italy. For the study area, we prepare a multi-temporal inventory map through the interpretation of multiple sets of aerial photographs taken between 1955 and 1999. We partition the basin into 2243 geo-morpho-hydrological units, and obtain the probability of spatial occurrence of landslides by discriminant analysis of thematic variables, including morphological, lithological, structural and land use. For each mapping unit, we obtain the landslide recurrence by dividing the total number of landslide events inventoried in the unit by the time span of the investigated period. Assuming that landslide recurrence will remain the same in the future, and adopting a Poisson probability model, we determine the exceedance probability of having one or more landslides in each mapping unit, for different periods. We obtain the probability of landslide size by analysing the frequency–area statistics of landslides, obtained from the multi-temporal inventory map. Assuming independence, we obtain a quantitative estimate of landslide hazard for each mapping unit as the joint probability of landslide size, of landslide temporal occurrence and of landslide spatial occurrence. 相似文献
14.
本文旨在更好地解读国家政策与移民流动性之间的相互关系。基于门槛分析方法,我们建立了关于边界、流动性和移民的基础理论,并重点探讨了具有移民倾向的个体心理过程。人们往往根据以下3个地理门槛作出移民抉择：一是关注迁移、离开熟悉的地方、跨越国界的想法;二是关注目的地区位及其边界和“接壤”(Bordering);三是关注迁移路径或途径。本文的案例主要来自欧盟和东南亚国家,分别包括荷兰和德国之间的跨界现象,2008年经济危机后欧盟的人口流动,2015-2016年期间欧盟和土耳其间的难民流动,菲律宾劳工移民,以及印度尼西亚—马来西亚迁徙通道等。最后,本文讨论了流动性和边界政策及治理。 相似文献
15.
京津冀城市群城镇化与创新的耦合过程与机理 总被引：2，自引：1，他引：2
城市群是国家新型城镇化的主体形态,也是创新的孵化器;城市群区域的城镇化子系统与创新子系统之间理论上存在复杂交互关系。京津冀城市群是国家新型城镇化规划确定的国家级城市群,并将“全国创新驱动经济增长新引擎”作为其核心功能定位,因此有必要探索京津冀城市群的城镇化过程与创新发展之间的耦合关系,这对理解城镇化与创新之间的关系和京津冀城市群的发展问题都有裨益。通过梳理城镇化与创新两个子系统之间的内在理论关系,构建城镇化与创新的综合评价指标体系,借助耦合协调度模型和地理探测器因子探测方法,分析京津冀城市群城镇化与创新两子系统之间的耦合协调关系演变过程及作用机理。研究发现：① 京津冀城市群城镇化和创新的综合水平都呈现稳步增长的趋势,城镇化与创新的耦合协调关系总体向好的方向发展,但综合水平和耦合关系的空间差异都较大;② 创新滞后是京津冀城市群城镇化与创新耦合协调水平提升的关键阻力,近年京津冀城市群地区及多数城市表现为创新滞后的耦合协调类型;③ 京津冀城市群城镇化与创新的交互影响非常显著,特别是经济城镇化和社会城镇化对创新的影响、创新资源对城镇化的影响表现比较突出。 相似文献
16.
首次从化学工程的角度 ,将盐田系统作为一类特殊的化学反应器和无机盐分离设备进行了详细的论述。在大量试验基础上 ,系统地分析和研究了 Na+,K+,Mg2 +∥Cl-,- H2 O四元水盐体系卤水在天然蒸发状态下的宏观蒸发动力学参数。从理论上对与卤水蒸发相关的多种参数进行了分析和合理简化 ,概述了卤水蒸发过程中的质量传递规律。并在此基础上通过计算机模拟方法建立了四元水盐体系高浓度卤水在特定地域中进行天然蒸发的卤水宏观蒸发动力学模型 ,证明了多种简化和理论假设的合理性。对该数学模型在盐湖卤水开发中的盐田设计、盐田生产的现代化自动管理和控制等进行了探讨。在卤水蒸发动力学模型建立的过程中 ,针对实际生产过程的需要 ,通过多种参数的分析 ,建立了多种参数关系 相似文献
17.
Precipitation is an important component of global water and energy transport and a major aspect of climate change. Due to the scarcity of meteorological observations, the precipitation climate over Tibet has been insufficiently documented. In this study, the distribution of precipitation during the rainy season over Tibet from 1980 to 2013 is described on monthly to annual time scales with meteorological observations. Furthermore, four precipitation products are compared to observations over Tibet. These datasets include products derived from the Asian Precipitation-Highly-Resolved Observational Data(APHRO), the Global Precipitation Climatology Centre(GPCC), the University of Delaware(UDel), and the China Meteorological Administration(CMA). The error, relative error, standard deviation, root-mean-square error, correlations and trends between these products for the same period are analyzed with in situ precipitation during the rainy season from May to September. The results indicate that these datasets can broadly capture the temporal and spatial precipitation distribution over Tibet. The precipitation gradually increases from northwest to southeast. The spatial precipitation in GPCC and CMA are similar and positively correlated to observations. Areas with the largest deviations are located in southwestern Tibet along the Himalayas. The APHRO product underestimates, while the UDel, GPCC, and CMA datasets overestimates precipitation on the basis of monthly and inter-annual variation. The biases in GPCC and CMA are smaller than those in APHRO and UDel with a mean relative error lower than 10% during the same periods. The linear trend of precipitation indicates that the increase in precipitation has accelerated extensively during the last 30 years in most regions of Tibet. The CMA generally achieves the best performance of these four precipitation products. Data uncertainty in Tibet might be caused by the low density of stations, complex topography between the grid points and stations, and the interpolation methods, which can also produce an obvious difference between the gridded data and observations. 相似文献
18.
现象学着重关注人的经验问题。在绅士化失所研究领域里,当研究视角从关注物质空间转变为空间经验时,“生活世界”成为了基本的出发点,这体现为从“直接性失所”往“间接性失所”的转变。以列斐伏尔的“表征的空间”为基础,围绕象征要素对失所经验展开定性分析则成为主要的研究路径。以此方法论,对重庆市下浩历史文化社区经历绅士化凸显出的失所经验进行分析,发现：1）失所经验在社区原住民、移民与游客群体中具有不同的表现方式。原住民的失所经验体现为其世代传承地方要素的丧失,导致“存在内部性”的丧失;移民的失所经验表现为移情载体的消失,导致其自由生活方式的丧失;游客的失所经验体现为彻底商业化导致其寻根体验地的消亡。2）移民在社区中开展的文化商业活动起到了嫁接内部本真社会空间与外部消费空间的作用,导致本真“社会空间”被中产阶级消费空间所置换。 相似文献
19.
“丝路”海运网络的脆弱性及风险控制研究 总被引：3，自引：0，他引：3
为研究海上丝绸之路集装箱海运网络的脆弱性,对沿线集装箱港口及挂靠航线进行了统计,构建了海上丝绸之路集装箱海运网络,以随机攻击和蓄意攻击两种方式分别对网络的平均度、孤立节点比例、聚类系数、平均路径长度、网络效率和最大连通子图相对大小等反映网络连通性特征值的变化进行了研究。结果表明“丝路”海运网络在受到随机攻击时较为“强壮”,在受到蓄意攻击时相对脆弱。经进一步挖掘,揭示了蓄意攻击下网络开始崩溃和完全崩溃的临界点,并据此指出了需重点保护的枢纽干线港;结合地理特征,分析了“丝路”中主要海上通道通航受阻时网络连通性的变化,发现马六甲海峡、台湾海峡、曼德海峡及苏伊士运河对网络的脆弱性影响最为显著。为进行风险评价,分析了“丝路”网络脆弱性形成因素和抗毁性机制,并提出了相应的抗毁性评价方法,经计算得出南亚为“丝路”网络中抗毁性最薄弱的区域。最后,结合地缘风险分析,提出了相应的对策和建议。本研究对于认清“丝路”海运网络的脆弱性及风险控制方法,保障其互联互通,具有重要的理论意义和应用价值。 相似文献
20.