Weathering, shock metamorphism and type distribution patterns of 98 ordinary chondrites from the Grove Mountains, Antarctica

Petrography and mineral chemistry of ninety-eight ordinary chondrites from Grove Mountains (GRV), Antarctica, were presented and their.weathering effect, shock metamorphism and type distribution patterns were discussed in this study. Among them, six are unequilibrated ordinary chondrites, including 3 H3 and 3 L3; and 92 meteorites are equilibrated ordinary chondrites, including 24 H-group (13 H4, 10 H5, 1 H6), 64 L-group (2 L4, 44 L5, 18 L6) and 4 LL-group (3 LL4, 1 LL5). Most GRV chondrites (>90%) displayed minor weathering effect (W1 and W2). About half of the meteorites experienced severe shock metamorphism. They commonly contain shock-induced melt veins and pockets. These heavily shocked meteorites provide us with natural samples for study of high-pressure polymorphs of minerals. In addition, the Grove Mountains collection seems to have more abundant unequilibrated and L group ordinary chondrites compared to the US Antarctic meteorite collection which were mainly found along the Transantarctic Mountains.     

贵州省拐卖儿童犯罪的多维时空格局及影响因素研究

拐卖儿童犯罪作为一种影响恶劣的社会现象,已引起公众和学界的广泛关注。基于犯罪地理学视角的相关研究起步较晚且侧重宏观分析,当前亟须聚焦犯罪热区作精细解析。本文以中国拐卖犯罪主要源区贵州省为研究区,采用文本分析、数理统计、空间计量等方法,揭示被拐儿童的社会人口学特征及拐卖儿童犯罪的多维时空格局与影响因素。结果表明：① 1~6岁男童为核心受害对象,拐卖导致的儿童迁移以城乡间交叉流动为主。② 犯罪在1944—2018年间呈“中段高发、首尾低发”态势,空间上集中于贵州西北半壁,尤以贵阳为最,微观地点上高发于人员流动频繁的开放型空间。③ 犯罪路径以“黔入东部”和“川滇入黔”为主,以省内跨市流动为辅。④ 犯罪主要受人口自然变动、生育政策、流动人口和经济发展水平等的影响。     

The Influence of Wind Speed and Sea States on Whitecap Coverage

Callaghan and White(2009) put forward the automated whitecap extraction(AWE) technique to determine the whitecap coverage(W). An improved AWE was used to analyze images collected in the South China Sea during 2012 and 2013 and in western Pacific during 2015 to determine W. The influences of meteorological and oceanographic factors on whitecap coverage were investigated in this study. It is found that W increases with wind speed. Scale factor and exponent of parameterization for W(U10) vary greatly in different models. Overall, there is a larger scatter of W at low wind speed than at high wind speed. W decreases with the increasing of wave age. Compared with wind speed, the scatter of W is smaller with wave age, which means the impact of wave age on the whitecap coverage is more robust under various environmental conditions. There is no significant dependence on SST and whitecap coverage seems to weakly decrease with SST. W decreases with the atmospheric stability. Relationship between W and wind speed change when swells are dominant. Swell can suppress wave breaking and decrease W. The effect is independent of the deflection angle between wind wave and swell.     

Distribution patterns of gypsum and kalistrontite in a dry lake basin of the southwestern Kalahari (Omongwa pan,Namibia)

The deposits of the Omongwa pan, southwestern Kalahari, Namibia, are partly gypsiferous and locally contain small amounts of kalistrontite. The distribution patterns of gypsum (CaSO₄.2H₂O) and kalistrontite (K₂Sr(SO₄)₂) are mainly determined by groundwater depth and by the lithological composition of the deposits. The latter determines the hydraulic conductivity for saturated and unsaturated flow and therefore controls the depth of the interval within the deposits where evaporation and mineral precipitation can take place. Other factors that affect the distribution of the evaporite minerals are the patterns of groundwater flow within the basin and the occurrence of a redistribution of salts during short flooding stages. Gypsum occurs as crystals of four distinct morphological types, which each developed in different conditions: prismatic crystals formed both as subaqueous precipitates and as crystals that developed within the sediment matrix of a brine-saturated surface layer; sub/euhedral tabular crystals formed within brine-filled macropores; hemi-bipyramidal crystals formed in a nearly permanently brine-saturated part of a subsurface horizon (phreatic zone), as the product of recrystallization of an older gypsum occurrence; and lenticular crystals formed by intrasediment growth in the vadose zone. The development of these morphological types of gypsum crystals is marked by differences in the differential inhibition of growth of the various crystal forms. The further growth of lenticular crystals, which are most strongly affected by differential growth inhibition, is still characterized by a difference in degree of inhibition between the {1 11} and {1 03} forms, expressed as a change in orientation of the plane of flattening. Copyright © 1999 John Wiley & Sons, Ltd.     

西藏拉鲁湿地浮游植物群落时空分布特征及其驱动因子

为了解西藏拉鲁湿地浮游植物群落时空分布特征及其驱动因子,于2021年7月、10月和2022年5月在拉鲁湿地主要水系进行定性和定量样品采集,共采集浮游植物水样126个,从不同季节和不同生境浮游植物种类组成、多样性等方面入手,探讨拉鲁湿地浮游植物群落时空分布特征及其驱动因子,为研究拉鲁湿地生态系统和稳定发展提供基础资料。结果表明:1)拉鲁湿地共鉴定出浮游植物532种(含变种和变型),隶属于8门13纲36目74科130属,物种组成表现为硅藻-绿藻-蓝藻型。2)拉鲁湿地浮游植物群落特征参数在不同季节和不同生境之间存在差异。夏季浮游植物群落的Shannon-Wiener多样性指数显著高于秋季和春季,Simpson优势度指数显著高于秋季。秋季浮游植物群落的Pielou均匀度指数显著低于夏季和春季。春季浮游植物群落的Margalef丰富度指数显著低于夏季和秋季。沼泽生境的浮游植物群落的Margalef丰富度指数显著高于湿草甸生境。3)季节是浮游植物群落组成差异的关键因素,生境对浮游植物群落组成的影响较弱,夏季的距离衰减模式比秋季和春季更强。4)拉鲁湿地不同的浮游植物群落参数与不同环境因子之间存在显著的关联。5)空间因素在解释浮游植物群落变异方面具有显著贡献,而快速变化的水质变量在决定浮游植物的季节变化中起着重要作用。季节和缓慢变化水质因子的解释能力相对较弱,但仍对浮游植物群落的变异有一定影响。     

整合DMSP/OLS和NPP/VIIRS夜间灯光遥感数据的长江三角洲城市格局时空演化研究

本文基于1992-2012年DMSP/OLS和2012-2018年NPP/VIIRS夜间灯光遥感数据,对长江三角洲城市群时空演化格局进行监测.考虑到不同卫星夜间灯光遥感数据之间的不一致性以及城市核心区亮度过饱和问题,对DMSP/OLS和NPP/VIIRS数据进行连续性校正、去饱和处理和一致性校正,构建长江三角洲区域19...     

河控三角洲生长的动力和沉积模式

分析河口动力特征,进而揭示其控制下的三角洲前缘挟沙河流床沙载荷(推移质)搬运和沉积机制,是合理构建河控三角洲生长沉积模式的前提.运用流体力学的湍流理论从微观动力过程角度分析失去河床约束条件下依靠惯性作用流动的河水入湖过程中河、湖两类水体的相互作用机制及流动规律,结合水槽物理模拟及前人开展的数值模拟,并借鉴河流泥沙动力学...     

基于资源环境数据格网化表达的关联模式发现

传统空间关联模式以空间谓词作为发现逻辑进行知识发现,会导致关联模式侧重空间位置关联,并且挖掘结果受所建立谓词表的限制,存在所发现模式固定、解释自由度差等问题。本文提出一种不依赖于空间谓词的关联模式发现方法,该方法将空间数据进行格网化表达,对格网化结果以平滑移动的N×N掩膜进行多约束事务化,将传统Apriori算法去除属性自连接,然后对所构建的空间事务化数据库进行关联模式探索,抽取有价值的关联模式。最后,以山西省晋城市长河流域为实证研究区,建立煤、地、水空间事务数据库,给出格网化表达的定量误差,探索其隐含空间关联模式,并以同位模式验证了事务化结果的精度。格网化生成覆盖研究区的64 m格网28 434个,各数据层格网化误差均在5%以内,以耕地为主因子事务化结果共有记录38 310条记录。对抽取的部分关联模式分析表明：发现结果符合长河流域矿农复合区背景下耕地相关的先验知识;该方法能有效提取空间数据及其属性信息中潜在的关联模式,提高了挖掘过程自由度和结果的兴趣度。     

台湾海峡风涌浪分离方法研究

受狭管效应的影响,台湾海峡波浪较大且常与涌浪混合存在。涌浪对包括船舶在内的浮式结构物有着重要的影响,而风涌浪分离是研究涌浪特性的必要前提,也一直是研究的热点和困难问题。由于数据的欠缺和观测条件的限制,在风涌浪分离方法中被普遍认可的二维谱方法常常难以使用,如何选择更为精准的一维谱方法往往会成为实际研究和应用过程中必须面对的问题。利用台湾海峡内3个具有二维谱数据的测站,通过将二维谱分离结果作为参考,针对台湾海峡风浪和涌浪的特征,探讨了风涌浪分离一维谱方法在该海域的适用性问题,研究表明风速法相较其他方法精度更好,在这一基础上提出了一种将波谱积分法与风速法相结合的一维谱方法。