临沂市农村集体建设用地流转成效探析

随着经济的快速发展,国有建设用地日渐稀缺,而同时集体建设用地在经历了20世纪90年代末期乡镇企业的没落之后出现大量的闲置。因此,建立规范的农村集体建设用地市场,引导集体建设用地合法、有序流转是激发农村地区经济活力、缓解国有建设用地紧张的重要举措。临沂市自2003年开始试点农村集体建设用地流转工作,在长期的实践中取得了一定的成绩,但也出现了一系列问题。该文在总结了临沂市农村集体建设用地流转工作经验的同时,对实践中发现的一系列问题进行分析、探索,提出了促进农村集体建设用地流转的措施与建议。临沂市自2003年开始试点农村集体建设用地流转工作,至2013年临沂市农村集体建设用地流转1 425.17 hm~2,获得流转收益19 827.01万元。结合临沂市的现实状况和我国农地入市改革的推进情况,最终从顶层设计、严格执法、市场化运作、规划布局、分配机制构建等方面提出促进农村集体建设用地流转的措施与建议。     

模糊数学在海（咸）水入侵水质评价中的应用—以寿光地区为例

运用模糊数学的基本思想方法,结合海(咸)水入侵的特点,依据寿光地区2015年丰水期地下水水质监测结果,选取Cl-、矿化度、咸化系数、钠吸附比等4项水化学指标作为评价因子,构建模糊综合评价数学模型,对寿光海(咸)水入侵现状进行了模糊综合评价,并验证了此模糊综合评价结果的可靠性。     

山东枣庄杨家堡子铁矿床地质特征及成因探讨

杨家堡子铁矿位于山东省枣庄市峄城区峨山镇,隶属苍峄铁成矿带,矿体赋存于新太古代泰山岩群山草峪组上部的变质岩中。该矿床内圈定磁铁矿体11个,求得铁矿石(333)资源量3 378.2万t,矿床平均品位TFe 33.30%,mFe 22.64%。主矿体为Ⅲ-6矿体,占矿床总资源量的83.69%,其长度1 137 m,最大斜深1 065 m,埋深707~1 369m,形态复杂程度中等,品位变化属均匀类型。含矿岩石为磁铁石英角闪岩。矿石中的主要有用组分为Fe,伴生元素含量较低,均无综合回收利用价值,有害组分S、P的含量均较低,经选矿后可达到炼钢及炼铁要求。矿石结构主要有粒状变晶结构和柱状变晶结构;矿石的构造主要为条带状构造,块状构造的矿石较少,但品位相对较高。矿石自然类型为原生磁铁矿石,工业类型属需选磁性铁矿石。该矿床成因与苍峄铁矿一脉相承,为典型的BIF型铁矿。根据区内以及邻区的见矿情况结合磁异常特征分析,杨家堡子矿区有良好的找矿前景。     

多边形自动构面算法的实现与优化

多边形自动构建是空间拓扑关系建立的难点和重点,效率受到多方面因素制约。在分析基于最小角法则的多边形自动搜索算法的基础上,在关联线段、有效多边形、相同线段的筛选等方面进行了改进,优化了多边形搜索、重复多边形筛选以及特殊多变形处理等算法,解决了重复搜索、多边形筛选耗时过长、特殊多边形(桥连多边形)的错误等问题,整体上较大地提高了多边形自动构面的效率,并在房产测绘的实际应用中得到验证。     

面向时空信息的智慧临沂建设实践

自智慧城市的概念提出以来,世界各国竞相开展智慧城市的研究和实践,国内各城市也迅速行动,纷纷开展智慧城市建设,以之作为转变发展方式、实现可持续发展的重要手段去推动。在智慧城市建设过程中,物联网、云计算、大数据、互联网+、移动互联等新技术取得了较大的发展进步和应用效果。该文在分析智慧城市概念和特征的基础上,介绍了测绘地理信息部门关于时空信息大数据和云平台建设的思路和关注点。梳理了智慧城市的总体框架,并对涉及的主要关键技术进行了分析。结合智慧临沂建设的实例,从基本情况、目标任务、主要内容、实现方式和实施进展等方面进行了详细介绍,并对智慧城市建设的重要作用进行了总结。智慧城市建设是一项复杂的系统工程,适合该地实际,能够切实解决该地实际问题的建设模式,才是智慧城市应该首要考虑的问题。     

耕地资源数量变化与城镇化水平协同性关系研究——以合肥市为例

城镇化是衡量一个国家和地区工业化和现代化的重要标志,是实现区域社会经济增长、促进地区和谐发展的战略决策。随着城镇化水平的不断提升,合肥市耕地非农化速度过快、耕地资源数量大幅降低等现实问题凸显,导致城镇化发展与耕地保护之间的关系日趋复杂,进一步加剧了社会经济发展与耕地资源保护二者之间的矛盾。适时开展耕地资源数量变化与城镇化协同性关系研究,深入挖掘城镇化过程中耕地资源数量变化的内在规律,对于妥善处理经济发展与耕地保护、持续推动区域新型城镇化建设具有重要的理论价值和现实意义。     

Formation and evolution of Emeishan basalt saprolite in vadose zones of Touzhai landslide source rockmass

In order to explain the formation process of slope hazards, and to identify the key factors leading to instability of a slope, Emeishan basalt saprolite in vadose zones of the Touzhai landslide in Zhaotong, Yunnan, was studied. The formation and evolution of Emeishan basalt saprolite was examined using, amongst other techniques, field investigations, thin section analysis, scanning electron microscopy (SEM) observations, chemical analysis, physical and water-physical property tests of rock masses. Field observations revealed that the majority of the weathered rock blocks were presented as a concentric layer structure in which an internal corestone was enveloped with several layers of external saprolized crust. Chemical and mineralogical analysis identified that iron was the most sensitive element and that the weathering progress usually started with the oxidation of Fe²⁺ to Fe³⁺ in rock blocks. Alkaline elements such as Si, Ca, Mg, Na and K were also dissolved and Fe and Al were concentrated in saprolized crusts. Results indicated that loss on ignition (LOI) also increased significantly. SEM results showed that the weathering intensity of the basalt blocks decreased gradually from the outside to the inside, and the mineral morphology significantly differed on both sides of the weathering front. The saprolized crusts presented cellular microstructure features due to the generation of micropore and clay minerals. Thin section analysis showed that plagioclase was relatively more stable than pyroxene and chlorite during weathering. With a centripetal propagation of the weathering front, saprolized crusts became thicker and corestones became smaller; fresh Emeishan basalt blocks gradually turned into saprolized blocks. Due to the loose structure and low strength of saprolite, the quality of the Emeishan basalt mass significantly deteriorated, this being a potentially important factor which caused the Touzhai landslide to occur.     

Global water vapor content decreases from 2003 to 2012: An analysis based on MODIS data

Water vapor in the earth′s upper atmosphere plays a crucial role in the radiative balance, hydrological process, and climate change. Based on the latest moderate-resolution imaging spectroradiometer(MODIS) data, this study probes the spatio-temporal variations of global water vapor content in the past decade. It is found that overall the global water vapor content declined from 2003 to 2012(slope b = –0.0149, R = 0.893, P = 0.0005). The decreasing trend over the ocean surface(b = –0.0170, R = 0.908, P = 0.0003) is more explicit than that over terrestrial surface(b = –0.0100, R = 0.782, P = 0.0070), more significant over the Northern Hemisphere(b = –0.0175, R = 0.923, P = 0.0001) than that over the Southern Hemisphere(b = –0.0123, R = 0.826, P = 0.0030). In addition, the analytical results indicate that water vapor content are decreasing obviously between latitude of 36°N and 36°S(b = 0.0224, R = 0.892, P = 0.0005), especially between latitude of 0°N and 36°N(b = 0.0263, R = 0.931, P = 0.0001), while the water vapor concentrations are increasing slightly in the Arctic regions(b = 0.0028, R = 0.612, P = 0.0590). The decreasing and spatial variation of water vapor content regulates the effects of carbon dioxide which is the main reason of the trend in global surface temperatures becoming nearly flat since the late 1990 s. The spatio-temporal variations of water vapor content also affect the growth and spatial distribution of global vegetation which also regulates the global surface temperature change, and the climate change is mainly caused by the earth's orbit position in the solar and galaxy system. A big data model based on gravitational-magmatic change with the solar or the galactic system is proposed to be built for analyzing how the earth's orbit position in the solar and galaxy system affects spatio-temporal variations of global water vapor content, vegetation and temperature at large spatio-temporal scale. This comprehensive examination of water vapor changes promises a holistic understanding of the global climate change and potential underlying mechanisms.     

鲜水河断裂带的构造大地测量

利用短边GPS点阵、短基线标石阵和精密激光测距 ,在与鲜水河断裂带的断层破裂带垂直的剖面上和构造盆地内进行构造大地测量 ,获得了断层软弱带和断层蠕变带上的最佳形变分布。综合利用相关地学成果和理论 ,揭示了构造形变所隐含的动力学信息 ,识别了断层应变带、塑性流变带和主断面在地面的分布范围。用外围GPS远场联测成果探讨了该断裂带的驱动力机制 ,匡正了其“左旋”运动和现今活动速度的含义。最后 ,评估了该断裂的地震活动趋势     

定水头注水引起的含水层水平运动和应变

基于含水层固体颗粒与孔隙水不可压缩的假设 ,本文导出了单井注水情况下泰斯承压含水层水平运动速度与水头之间的基本关系式。然后利用注水井壁处的应力、应变边界条件 ,进一步导出了单井定水头注水引起的泰斯承压含水层水平运动速度、位移和应变解析表达式。该水平位移与应变由两部分组成 :一部分为由注水压力本身引起的经典弹性力学解项 ,它仅随半径而变化 ,与注水时间无关 ;另一部分为由地下水头变化引起的水动力学位移和应变解项。其中 ,含水层水动力学水平位移随时间加长呈指数增长特征 ,水动力学径向应变则表现为近井处拉张、远井处挤压的分区特征 ,且近井拉张区随时间加长逐渐向外扩展。单井注水含水层水动力学水平位移、应变解的导出 ,完善和发展了单孔内压经典弹性平面力学问题解