基于CA模型的旅游小镇增长的时空模拟与应用——以河北三坡镇为例

旅游小镇增长的时空模拟是城镇化影响下的土地利用/覆盖变化研究的重要手段。近年来旅游小镇的城镇化以其旅游业发展带动城镇发展的独特模式引起国内外学者的高度关注。论文以元胞自动机模型为基础,运用旅游小镇旅游城镇化增长模型,对河北省三坡镇的旅游城镇化发展进行模拟与预测。模拟结果显示:①2005-2010年研究区城镇增长主要围绕现有镇区范围扩展,全域年均增速为0.015 km²/年;②2010-2015年主要城镇增长区位于镇内距离景区较近的苟各庄村附近,全域年均增速为0.040 km²/年,其他区域则保持相对较为平稳的状态。研究表明元胞自动机模型在模拟旅游小镇演化具有较高的可靠性,为研究城镇化条件下区域生态景观格局变化提供前提保证,对于提高土地资源利用效率,保障小镇健康有序发展具有十分重要的意义。     

利用船测数据以及Landsat-7 ETM+影像评估南极海冰区AMSR-E海冰密集度

利用第26次中国南极科学考察期间收集的海冰密集度船基观测资料以及由Landsat-7 ETM+得到的海冰密集度来验证AMSR-E南极海冰区海冰密集度产品的精度。AMSR-E海冰密集度与船基目视观测的海冰密集度存在着一定的线性关系(R²=0.816), 但两者匹配得并不是很好。与ETM+海冰密集度相比,AMSR-E数据趋向于低估海冰密集度,在25景晴空条件下的ETM+影像中,平均海冰密集度偏差(AMSR-E海冰密集度-ETM+海冰密集度)从-5.33%到-21.5%,而相应的均方根误差RMSE (Root Mean Squared Errors)从13.7%到33.8%。依据Landsat-7 ETM+ 海冰分类,AMSR-E数据海冰密集度最大的误差产生于新冰区。     

Spatio-temporal data model based on relational database system

In this paper, the entity-relation data model for integrating spatio-temporal data is designed. In the design, spatio-temporal data can be effectively stored and spatiao-temporal analysis can be easily realized.     

Aerosol-Cloud-Precipitation Interactions in a Closed-cell and Non-homogenous MBL Stratocumulus Cloud

A closed-cell marine stratocumulus case during the Aerosol and Cloud Experiments in the Eastern North Atlantic (ACE-ENA) aircraft field campaign is selected to examine the heterogeneities of cloud and drizzle microphysical properties and the aerosol-cloud-precipitation interactions. The spatial and vertical variabilities of cloud and drizzle microphysics are found in two different sets of flight legs: Leg-1 and Leg-2, which are parallel and perpendicular to the cloud propagation, respectively. The cloud along Leg-2 was close to adiabatic, where cloud-droplet effective radius and liquid water content linearly increase from cloud base to cloud top with less drizzle. The cloud along Leg-1 was sub-adiabatic with lower cloud-droplet number concentration and larger cloud-droplet effective, but higher drizzle droplet number concentration, larger drizzle droplet median diameter and drizzle liquid water content. The heavier drizzle frequency and intensity on Leg-1 were enhanced by the collision-coalescence processes within cloud due to strong turbulence. The sub-cloud precipitation rate on Leg-1 was significantly higher than that along Leg-2. As a result, the sub-cloud accumulation mode aerosols and CCN on Leg-1 were depleted, but the coarse model aerosols increased. This further leads to a counter-intuitive phenomenon that the CCN is less than cloud-droplet number concentration for Leg-1. The average CCN loss rates are ?3.89 \begin{document}$\mathrm{c}{\mathrm{m}}^{-3}\;{\mathrm{h}}^{-1}$\end{document} and ?0.77 \begin{document}$\mathrm{c}{\mathrm{m}}^{-3}\;{\mathrm{h}}^{-1}$\end{document} on Leg-1 and Leg-2, respectively. The cloud and drizzle heterogeneities inside the same stratocumulus can significantly alter the sub-cloud aerosols and CCN budget. Hence it should be treated with caution in the aircraft assessment of aerosol-cloud-precipitation interactions.     

Effects of land cover type conversion on water exchange and climate change in the source area of the Yellow River

Theoretical and Applied Climatology - The surface radiation and energy flux in the source area of the Yellow River are estimated by using the Moderate Resolution Imaging Spectroradiometer products...     

咸阳城区热储流体混合作用研究及模拟计算

应用水文地球化学模拟方法对咸阳城区热储流体混合作用分析和混合比例的计算.结合研究区的地热地质和水文地质条件,进行地下热水混合作用和混合程度的研究.结果表明,咸阳城区地下热水在不同程度上都存在与较低温度地下热水的混合作用。应用PHREEQC模拟软件、稳定同位素D和温度计算热水与冷水的混合比例,估算在平衡条件下咸阳城区地下热水与冷水的混合比例在0.09～0.63之间。     

油气输导体系研究现状及存在问题的探讨

油气输导体系是油气成藏体系的必要元素,也是油气运移研究的薄弱环节。人们对于这一概念的阐述各不相同,绝大多数学者将其划分为高孔渗砂体、断层及裂缝、不整合面以及它们两两或全部的复合输导体系四种类型,目前对输导体系的研究也集中在这四种类型上。对高孔渗砂体的研究主要集中在孔隙结构、渗透率和优势运移通道上;对断层的研究主要集中在断层泥、非渗透性物质、两盘特征、断层面应力及断层活动性上;对不整合面的研究主要集中在其产状、性质、类型及岩性组合等方面。输导体系的类型划分应当以渗透率非均质性为依据,同时充分考虑烃源岩。从盆地沉积演化的角度出发研究各类输导体系的分布,也是油气运移研究领域中的薄弱环节。     

新疆天山成矿带铁磷矿地质及成矿专属性

本文对成矿带内的岩浆岩杂岩体进行了含矿性研究,划分出4个含矿杂岩带与5个矿床成因类型。成矿专属性研究表明:岩浆岩型铁磷矿受古地台边缘深大断裂控制;容矿岩石为主要偏碱性-铁质及铁镁质岩系列;容矿岩石主微量元素明显不和谐;岩石类型共生组合主要表现为黑云母透辉石岩、辉石岩、碱性辉长岩、斜长岩、碳酸岩的共伴生;矿物共生组合主要表现为透辉石+磷灰石+磁铁矿+黑云母,斜长石+磷灰石+磁铁矿+钠黝帘石组合,辉石+磷灰石+磁铁矿等特征;元素的共生组合主要表现为P、Fe、Ti、V、REE具显著相关性。通过预测研究,进行了找矿远景区的划分,划分出具有成矿条件的9个找矿远景区。     

西昆仑康西瓦断裂西段斜长片麻岩LA-ICP-MS锆石U-Pb定年及其构造意义

在康西瓦断裂西段发育着一套含石榴子石二云斜长片麻岩。根据锆石的阴极发光图像和Th、U、REE等特征,锆石可分为岩浆成因和变质热液成因2类。利用LA-ICP-MS法进行锆石U-Pb定年,测得含石榴子石斜长片麻岩的源岩形成年龄为254.5Ma±4.2Ma(MSWD=0.16),变质年龄为242.7Ma±2.3Ma(MSWD=0.11)。结合区域地质资料,含石榴子石二云斜长片麻岩的变质作用与古特提斯碰撞造山有关,表明西昆仑造山带在中三叠世早期(243Ma)仍处于古特提斯碰撞造山期。     

滇西北兰坪盆地北部上三叠统含盐层位的厘定及其意义

通过野外实测剖面和大量室内岩矿工作,首次指出兰坪盆地上三叠统至少存在2套含盐层位,上含盐层位于三合洞组上段(T3s2),盐类物质以石膏、天青石为主,下含盐层位于三合洞组下段(T3s1),以天青石为主。天青石和石膏均呈中厚层层状产出,与顶底板地层产状一致。不同地区含盐层岩石组合及序列不同,横向上不具有可对比性,提出其并非正常蒸发沉积产物的认识。同时,含盐地层又是盆地内铅锌矿重要的赋矿层位,因此上三叠统含盐建造层序的厘定对深化认识区域铅锌矿床成矿机制、指导盐类矿床和铅锌矿找矿具有重要的意义。