兰州新区建设用地生态适宜性评价     

张胜武  申成磊  石培基  赵锐锋  姜朋辉  刘海猛 《中国沙漠》2014,34(5):1434-1440

在地理信息技术的支持下,修正单纯的权重叠加法,采用潜力-限制性分析法分析了兰州新区建设用地的生态潜力和生态阻力,对其生态适宜性做出科学评价,得到兰州新区可用作建设用地的理想区域。结果表明：（1）兰州新区建设用地开发的生态潜力总体以一级为主,二级次之,三级和四级区所占比重较小;（2）一级生态阻力主要分布在新区南部山地,主要表现为地形复杂、工程地质条件差、地质灾害发生频繁等;（3）兰州新区建设用地生态适宜性达一级的面积所占比重最大,为39 425.91 hm²,占新区总面积的48.91%。三级适宜区面积最小,仅为6 513.2 hm²,占新区总面积的8.08%。对应于生态适宜性评价结果,兰州新区土地应用可划分为集中建设区、重点开发区、限制建设区和禁止建设区。其中,集中建设区和重点建设区应为兰州新区建设用地开发的理想区域。  相似文献   

灾害学定义之下的土壤盐碱化风险评价   总被引：1，自引：0，他引：1  

谷洪彪  迟宝明  姜纪沂 《吉林大学学报(地球科学版)》2013,43(5):1623-1629

为改善灌区中低产地的产量、提高其田间管理及粮食综合生产能力、防止土壤盐碱化灾害的扩展,在土壤盐碱化灾害学研究的基础上,建立了土壤盐碱化灾害风险评价指标体系。选用基于熵权的灰色关联评价方法来构建土壤盐碱化灾害风险评价模型,根据标准自然灾害风险原理,建立土壤盐碱化灾害风险指数计算模型。在松原灌区土壤盐碱化灾害风险评价中的应用表明,灌区各灌片盐碱灾害风险值为0.10～0.36,属于中度风险和重度风险区,风险值由小到大排序为：前郭片、安字片、有字片、龙海片、水字片、大布苏片、潜字片、套浩太片、戎字片、红星片、洪字片。该模型与灌区实情符合较好,客观性较强,表明所建模型可用于土壤盐碱化灾害风险评价。  相似文献   

九江-瑞昌矿集区的3D结构及对区域找矿的启示   总被引：3，自引：2，他引：1  

邓震  吕庆田  严加永  赵金花  刘彦 《地球物理学报》2012,55(12):4169-4180

本文分析了九瑞地区重、磁场的分布特征.运用最新的方法技术对已有的重磁资料重新进行处理:采用重磁多尺度边缘检测方法,对九瑞矿集区区域重力和航磁数据进行了边缘检测,并根据检测结果重新厘定了断裂系统的展布位置.在整理、分析九瑞地区地质、地层物性资料的基础上,对实测的1∶5万重磁数据进行较细致的准三维反演.同时将重磁三维物性反演应用到岩浆岩空间结构研究中,获得了矿集区地层结构及岩浆岩三维空间形态特征.根据反演所得磁化率强弱,分析了岩体的基性程度,为寻找与火山岩、侵入岩体有关的金属矿产提供了指示信息.最终建立的模型给出了地下地层的分布特征、控矿构造的展布规律、与成矿相关岩体的三维形态以及已知矿点的空间分布特征,为在九瑞矿集区的深部寻找隐伏矿体提供了新的信息.  相似文献   

城市空间的生产——以近代上海江湾五角场地区的城市化为例   总被引：1，自引：1，他引：0  

张晓虹  孙涛 《地理科学》2011,31(10):1181-1188

城市地区景观的演变反映了人类活动对自然生态格局演替的人为干扰过程。由于人类活动的强度、频度及方式的差异,从半自然的农业生态景观演化为以人工建筑为主的城市生态景观的过程,可能呈现多样化的面貌。利用GIS技术将20世纪上半叶上海江湾五角场地区的土地利用状况逐年复原,发现其景观演变过程表现为由以农业生态景观为主转变为城乡景观杂错分布,并且这一进程因为各种政治事件的影响而呈现出明显的阶段性及空间差异性。揆诸史实,可知上海江湾五角场地区的城市化与城市空间的生产不仅是上海都市政治的产物,更是近代中国城市化的典型。  相似文献   

基于GIS和空间句法的历史街区保护更新规划方法研究—以江门市历史街区为例     

王成芳  孙一民 《热带地理》2012,32(2):154-159

基于GIS和空间句法集成的思路,以江门市历史街区保护更新规划为例,结合实地调研从空间实体的“点、线、面”3个层面分别建立建筑、街巷和地块GIS数据库,利用GIS多因子评价对建筑保护价值进行综合评价,运用空间句法定性定量的分析手段剖析历史街区的街巷路网结构及用地布局,尝试探索建立在量化、实证分析基础上的历史街区保护更新规划的技术方法和流程.研究结果表明:通过量算空间句法参数可以直观解析历史街区空间形态结构和智能性水平,对研究区的规划定位能提供较好的参考;通过空间句法与GIS集成分析对街巷和用地布局的合理性进  相似文献   

广西扶绥—崇左地区铝土矿矿产远景调查主要进展及成果          下载免费PDF全文

邓军  陈粤  黄宏伟  梁裕平  何海洲  陈胜  吴天生  杨志强  韦访  罗立营 《中国地质调查》2015,2(4):8-12

在龙州地区首次发现早石炭世的堆积型铝土矿矿源层,提出广西堆积型铝土矿至少存在早石炭世和晚二叠世两个时代的矿源层。探索运用高密度电阻率法寻找古风化壳沉积型铝土矿的有效性试验工作。提交新发现矿产地4处,探获新增铝土矿(334₁)资源量5 289.15万吨。重新厘定区域地层岩性及岩相特征,系统总结区内铝土矿矿床(点)的时空分布特征、控矿地质条件、成矿规律及找矿标志,建立了区域成矿模式和预测找矿模型,圈定成矿远景区5处,找矿靶区6处,开展区域矿产预测,初步评价了本区铝土矿资源潜力。为该地区下一步地质调查、矿产勘查规划和开发提供了丰硕的基础资料和有益参考。  相似文献   

Optimizing layout of pumping well in irrigation district for groundwater sustainable use in northwest China   总被引：1，自引：0，他引：1       下载免费PDF全文

Xin Liu  Sufen Wang  Zailin Huo  Fusheng Li  Xinmei Hao 《水文研究》2015,29(19):4188-4198

Optimizing layout of pumping well plays a vital role in curbing the groundwater level decline. A novel optimization model is presented in this study. First, the optimal well number is obtained by taking into account factors of local economy and environment based on nonlinear programming model. Then, the well spatial layout assessment model is attained based on information entropy weight and technique for order preference by similarity to ideal solution (TOPSIS). After that, the relative closeness to positive ideal solution of alternative (c_i) on the rationality of well spatial layout in cultivated land is calculated, and a set of alternatives are ranked according to the descending order of c_i. Finally, the well optimization layout is obtained by combining the optimal well number with well spatial layout assessment result based on the GIS data of pumping wells. As a case study, this method was applied in Yongchang Irrigation District of Shiyang River Basin, the arid region of northwest China. Results show that under the conditions of sustainable use of water resources, the irrigation district needed 724 wells for irrigation, with a decrease of 31.0% when compared with the existing number of wells. The wells with low flow rate and operating efficiency distributed in high density where groundwater is over‐exploitation were recommended to be closed. This well optimization layout method is expected to play a significant role in helping make plans for exploiting groundwater at more sustainable level, curbing the groundwater level decline trend, and improving the local ecological environment. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

Combined zircon and cassiterite U–Pb dating of the Piaotang granite-related tungsten–tin deposit,southern Jiangxi tungsten district,China     

《Ore Geology Reviews》2017

The large low-grade Piaotang W–Sn deposit in the southern Jiangxi tungsten district of the eastern Nanling Range, South China, is related to a hidden granite pluton of Jurassic age. The magmatic-hydrothermal system displays a zonation from an inner greisen zone to quartz veins and to peripheral veinlets/stringers (Five-floor zonation model). Most mineralization is in quartz veins with wolframite > cassiterite. The hidden granite pluton in underground exposures comprises three intrusive units, i.e. biotite granite, two-mica granite and muscovite granite. The latter unit is spatially associated with the W–Sn deposit.Combined LA-MC-ICP-MS U–Pb dating of igneous zircon and LA-ICP-MS U–Pb dating of hydrothermal cassiterite are used to constrain the timing of granitic magmatism and hydrothermal mineralization. Zircon from the three granite units has a weighted average ²⁰⁶Pb/²³⁸U age of 159.8 ± 0.3 Ma (2 σ, MSWD = 0.3). The cathodoluminescence (CL) textures indicate that some of the cassiterite crystals from the wolframite-cassiterite quartz vein system have growth zonations, i.e. zone I in the core and zone II in the rim. Dating on cassiterite (zone II) yields a weighted average ²⁰⁶Pb/²³⁸U age of 159.5 ± 1.5 Ma (2 σ, MSWD = 0.4), i.e. the magmatic and hydrothermal systems are synchronous. This confirms the classical model of granite-related tin–tungsten mineralization, and is against the view of a broader time gap of >6 Myr between granite magmatism and W–Sn mineralization which has been previously proposed for the southern Jiangxi tungsten district. The elevated trace element concentrations of Zr, U, Nb, Ta, W and Ti suggest that cassiterite (zone II) formed in a high-temperature quartz vein system related to the Piaotang granite pluton.  相似文献   

Magmatic–hydrothermal processes in Sangdong W–Mo deposit,Korea: Study of fluid inclusions and 39Ar–40Ar geochronology     

《Ore Geology Reviews》2017

The Sangdong scheelite–molybdenite deposit in northeast South Korea consists of strata-bound orebodies in intercalated carbonate-rich layers in the Cambrian Myobong slate formation. Among them, the M1 layer hosts the main orebody below which lie layers of F1–F4 host footwall orebodies. Each layer was first skarnized with the formation of a wollastonite + garnet + pyroxene assemblage hosting minor disseminated scheelite. The central parts of the layers were subsequently crosscut by two series of quartz veining events hosting minor scheelite and major scheelite–molybdenite ores, respectively. The former veins associate amphibole–magnetite (amphibole) alteration, whereas the latter veins host quartz–biotite–muscovite (mica) alteration. Deep quartz veins with molybdenite mineralization are hosted in the Cambrian Jangsan quartzite formation beneath the Myobong formation. In the Sunbawi area, which is in close proximity to the Sangdong deposit, quartz veins with scheelite mineralization are hosted in Precambrian metamorphic basement. Three muscovite ³⁹Ar–⁴⁰Ar ages between 86.6 ± 0.2 and 87.2 ± 0.3 Ma were obtained from M1 and F2 orebodies from the Sangdong deposit and Sunbawi quartz veins. The Upper Cretaceous age of the orebodies is concordant with the published ages of the hidden Sangdong granite, 87.5 ± 4.5 Ma. This strongly suggests that the intrusion is causative for the Sangdong W–Mo ores and Sunbawi veins.Fluid inclusions in the quartz veins from the M1 and F2 orebodies, the deep quartz-molybdenite veins, and the Sunbawi veins are commonly liquid-rich aqueous inclusions having bubble sizes of 10–30 vol%, apparent salinities of 2–8 wt% NaCl eqv., and homogenization temperatures of 180–350 °C. The densities of the aqueous inclusions are 0.70–0.94 g/cm³. No indication of fluid phase separation was observed in the vein. To constrain the formation depth in the Sangdong deposit, fluid isochores are combined with Ti–in–quartz geothermometry, which suggests that the M1 and F2 orebodies were formed at depths of 1–3 km and 5–6 km below the paleosurface, respectively. The similarity of the Cs (cesium) concentrations and Rb/Sr ratios in the fluid inclusions of the respective orebodies indicate an origin from source magmas having similar degrees of fractionation and enrichment of incompatible elements such as W and Mo. High S concentrations in the fluids and possibly organic C in the sedimentary source likely promoted molybdenite precipitation in the Sangdong orebodies, whereas the scheelite deposition in the deep quartz–molybdenite veins hosted in the quartzite is limited by a lack of Ca and Fe in the hydrothermal fluids. The molybdenite deposition in the Sunbawi quartz–molybdenite veins hosted in the Precambrian metamorphic basement rocks was possibly limited by a lack of reducing agents such as organic C.  相似文献   

蓄能式绳索取心液动潜孔锤的应用研究     

张飞 《地质与勘探》2017,53(6):1188-1196

蓄能式绳索取心液动潜孔锤钻具是在普通绳索取心钻具总成上端增加了发生和传递冲击载荷的结构,将冲击载荷通过绳索取心钻具外管传递至钻头。新疆达坂城黑沟-达拉地布拉克铀矿工区裂隙、构造蚀变带和构造破碎带发育,地层破碎,使用普通绳索取心钻具钻进,岩心极易堵塞、回次进尺短、频繁打捞内管、钻进效率极低。使用蓄能式绳索取心液动潜孔锤钻具钻进,增加了回次进尺,提高了钻进效率。论文依据施工现场使用情况,介绍了蓄能式绳索取心液动潜孔锤的结构和工作原理,统计、总结了应用情况,论述了绳索取心液动潜孔锤得出的应用结论。  相似文献