滇东南老君山中—深变质岩系铅同位素特征及时代归属

滇东南老君山地区是我国重要的锡多金属成矿区之一 ,区内中—深变质岩系的时代归属尚存在不同认识。通过对其中的花岗片麻岩类的铅同位素研究 ,获得全岩 长石铅 铅等时线年龄为 598±84Ma,( 2 0 7Pb/ 2 0 4 Pb) 0 =1 4 .52 3± 0 .2 3 5,γ =0 .97898,MSWD =1 4。这一年龄值代表了花岗片麻岩遭受混合岩化作用的年龄 ,相当于晚震旦世晚期。结合前人研究成果 ,本文认为该中—深变质岩系的时代归属于前寒武纪。     

Residues of selected antibiotics in water and mud from shrimp ponds in mangrove areas in Viet Nam

In recent years, antibiotics have been used widely in intensive shrimp culture and this may lead to their contamination of the environment. Surveys on residues of trimethoprim (TMP), sulfamethoxazole (SMX), norfloxacin (NFXC) and oxolinic acid (OXLA) in water and mud in shrimp ponds in mangrove areas were conducted in the north as well as in south of Viet Nam in July and August, 2002. The results show that these antibiotics are found in all samples in both shrimp ponds and surrounding canals. The highest concentrations of TMP, SMX, NFXC and OXLA are 1.04, 2.39, 6.06, and 2.50 ppm in water samples; and 734.61, 820.49, 2615.96, 426.31 ppm (based on wet mud weight), respectively. The comparison of antibiotics residues between study sites and types of shrimp ponds will be discussed in this paper. The results also suggest that antibiotics residues may cause harmful effect on ecosystems in the study sites.     

小麦冠层理化参量的高光谱遥感反演试验研究

以国产成像光谱仪所获高光谱遥感数据为基础，根据田间同步采样数据建立的基于反射光谱特征的小麦冠层生物物理和生物化学估计模型，实现了用航空高光谱遥感数据对田间小麦冠层理化参量的整体反演。结果表明：用高光谱遥感方法估计小麦冠层理化参量是可行的；以理化参数为“波段”的数字图像及其处理，为农学家以理化参量的空间分布及其差异解释作物产量空间分布差异和研究作物生态生理机理提供了新的手段。     

Spatial prediction models for shallow landslide hazards: a comparative assessment of the efficacy of support vector machines,artificial neural networks,kernel logistic regression,and logistic model tree

Preparation of landslide susceptibility maps is considered as the first important step in landslide risk assessments, but these maps are accepted as an end product that can be used for land use planning. The main objective of this study is to explore some new state-of-the-art sophisticated machine learning techniques and introduce a framework for training and validation of shallow landslide susceptibility models by using the latest statistical methods. The Son La hydropower basin (Vietnam) was selected as a case study. First, a landslide inventory map was constructed using the historical landslide locations from two national projects in Vietnam. A total of 12 landslide conditioning factors were then constructed from various data sources. Landslide locations were randomly split into a ratio of 70:30 for training and validating the models. To choose the best subset of conditioning factors, predictive ability of the factors were assessed using the Information Gain Ratio with 10-fold cross-validation technique. Factors with null predictive ability were removed to optimize the models. Subsequently, five landslide models were built using support vector machines (SVM), multi-layer perceptron neural networks (MLP Neural Nets), radial basis function neural networks (RBF Neural Nets), kernel logistic regression (KLR), and logistic model trees (LMT). The resulting models were validated and compared using the receive operating characteristic (ROC), Kappa index, and several statistical evaluation measures. Additionally, Friedman and Wilcoxon signed-rank tests were applied to confirm significant statistical differences among the five machine learning models employed in this study. Overall, the MLP Neural Nets model has the highest prediction capability (90.2 %), followed by the SVM model (88.7 %) and the KLR model (87.9 %), the RBF Neural Nets model (87.1 %), and the LMT model (86.1 %). Results revealed that both the KLR and the LMT models showed promising methods for shallow landslide susceptibility mapping. The result from this study demonstrates the benefit of selecting the optimal machine learning techniques with proper conditioning selection method in shallow landslide susceptibility mapping.     

青岛市水资源现状及保护对策

青岛市是我国严重缺水城市之一，水资源供需矛盾突出，形势十分严峻。从青岛市水资源的具体问题出发，对诸如地下水位下降、水质污染、海水入侵等问题进行具体和理论上的分析，并提出针对性的保护对策，在水资源的评价、开源与节流、区域水资源的开发利用、水污染防治与污水资源化及水资源的可持续利用等方面均提出新的观点，为青岛市水资源的可持续利用提供了科学的决策依据，对青岛市国民经济持续发展具有重要意义。     

Early Mesozoic lamprophyres in Gorny Altai: petrology and age boundaries

The Mesozoic Chuya dike complex was recognized by R.V. Obolenskaya based on the similar mineral composition of dikes and their age characteristics. Lamprophyres occur along the large Terekta–Tolbonur and Kurai–Kobda shear zones. The Chuya complex was studied by the example of two areas, South Chuya and Yustyd, with different levels of erosional truncation. The dikes of the first area are localized in the South Chuya Ridge, where they cut Cambrian–Ordovician metamorphic rocks, and the dikes of the Yustyd area occur in the Devonian terrigenous blackshale deposits of the Yustyd trough. The dikes of these areas differ in structures, textures, the degree of carbonatization, and mineral composition. The performed studies of rocks and minerals confirmed that the dikes of both areas belong to the same complex. They helped to establish the regularities of the lithologic composition of the entire complex and its local areas and to substantiate the recognition of areas not only from their geologic position but also by the composition, structures, and textures of rocks and their mineral composition. Geochronological data show two stages of the complex formation: 236–234 and 250–242 Ma. The results of studies also demonstrate that the lamprophyres and coeval syenites of the Tarkhata massif are fractionates of the same parental melt and can be united into a hypabyssal-plutonic complex. Comparison with other Permo-Triassic lamprophyre complexes showed that the wide variations of the composition of the Chuya rocks and its trend as well as the geochemical anomalies are specific features of complexes of high-K lamprophyres.     

Characteristic Features of REE and Pb–Zn–Ag Mineralizations in the Na Son Deposit,Northeastern Vietnam

The Na Son deposit is a small‐scale Pb–ZnPb–Zn–Ag deposit in northeast Vietnam and consists of biotite–chlorite schist, reddish altered rocks, quartz veins and syenite. The biotite–chlorite schist is intruded by syenite. Reddish altered rocks occur as an alteration halo between the biotite–allanite‐bearing quartz veins and the biotite–chlorite schist. Allanite occurs in the biotite–allanite‐bearing quartz veins and in the proximal reddish altered rocks. Rare earth element (REE) fluorocarbonate minerals occur along fractures or at rim of allanite crystals. The later horizontal aggregates of sulfide veins and veinlets cut the earlier reddish altered rocks. The earlier Pb–Zn veins consist of a large amount of galena and lesser amounts of sphalerite, pyrite and molybdenite. The later Cu veins cutting the Pb–Zn veins include chalcopyrite and lesser amounts of tetrahedrite and pyrite. The occurrences of two‐phase H₂O–CO₂ fluid inclusions in quartz from biotite–allanite‐bearing quartz veins and REE‐bearing fluorocarbonate minerals in allanite suggest the presence of CO₂ and F in the hydrothermal fluid. The oxygen isotopic ratios of the reddish altered rocks, biotite–chlorite schist, and syenite range from +13.9 to +14.9 ‰, +11.5 to +13.3 ‰, and +10.1 to +11.6 ‰, respectively. Assuming an isotopic equilibrium between quartz (+14.6 to +15.8 ‰) and biotite (+8.6 ‰) in the biotite–allanite‐bearing quartz vein, formation temperature was estimated to be 400°C. At 400°C, δ¹⁸O values of the hydrothermal fluid in equilibrium with quartz and biotite range from +10.5 to +11.7 ‰. These δ¹⁸O values are consistent with fluid that is derived from metamorphism. Assuming an isotopic equilibrium between galena (+1.5 to +1.7 ‰) and chalcopyrite (+3.4 ‰), the formation temperature was estimated to be approximately 300°C. The formation temperature of the Na Son deposit decreased with the progress of mineralization. Based on the geological data, occurrence of REE‐bearing minerals and oxygen isotopic ratios, the REE mineralization is thought to result from interaction between biotite–chlorite schist and REE‐, CO₂‐ and F‐bearing metamorphic fluid at 400°C under a rock‐dominant condition.     

人文主义地理学之我见

人文主义地理学出现于20世纪60年代末,是时欧美正涌动着人文主义思潮,它带动了对逻辑实证主义知识体系进行批判的一系列理论的出现,人文主义地理学就是其一。人文主义地理学的哲学基础是存在主义和现象学,段义孚和雷尔夫(Edward Relph)、布蒂默(Anne Buttimer)、莱(David Ley)、赛明思(Marvyn Samuels)和恩特里金(Nicholas Entrikin)等是人文主义地理学的代表人物。1976年段义孚发表了《人文主义地理学》一文,1978年这些学者一起出版了人文主义地理学的第一部论文集《人文主义地理学》。 　　人文主义地理学的一个主要目标是协调社会科学与人之间的关系,容纳知性(understanding)与智慧(wisdom),客观(objectivity)与主观(subjectivity)以及唯物主义和唯心主义。其主要任务是发展方法论,并深刻理解人类在世界所处的地位。本文各部分都渗透着这个主题。人文主义地理学的社会批判立足点是伦理和道德。 它强调人们对自然、对世界的感悟能力。本文从三个方面探讨了这种感悟力。第一,地理学关注不同地方的差异,地方之间的差异体现在各个地方特点的差异上。人们可以通过感官感受到地方,各种感受的综合形成了地方感;第二,人类在处理与自然的关系上往往是把强权加在自然之上,从而扭曲了自然的本来形态。感悟人与自然的和谐将提升人类的道德;第三,想象力是一种对世界的感悟能力,文化则是想象力的产物。人类在追求物质和精神生活时也会陷入怪圈。本文最后指出,人文主义地理学者必须能够把握大量的事实,同时洞悉人类对自然感悟的复杂与精妙。     

A coupled poroplastic damage model accounting for cracking effects on both hydraulic and mechanical properties of unsaturated media

Damage induced by microcracking affects not only the mechanical behaviour of geomaterials but also their hydraulic properties. Evaluating these impacts is important for many engineering applications, such as the safety assessment of radioactive waste disposal facilities. This paper presents a new constitutive model accounting simultaneously for the impact of damage on hydraulic and mechanical properties of unsaturated poroplastic geomaterials. The hydro‐mechanical coupling is formulated by means of the thermodynamic framework for partially saturated media, extended by taking into account isotropic damage and plasticity. State and complementary laws are governed by the so‐called plastic effective stress and equivalent pore pressure. Assuming a bimodal pore size distribution for cracked porous media, the hydraulic part (water retention curve and hydraulic conductivity) is modelled using phenomenological functions of damage variable. The participation of damage on both mechanical and hydraulic part enables this model to describe bilateral couplings between them. This coupled model is then validated against a number of experimental data obtained from Callovo‐Oxfordian argillite, which is the possible host rock for a radioactive waste disposal in France. Parametric studies are also carried out to check the consistency and to better demonstrate the bilateral couplings in the model. Copyright © 2015 John Wiley & Sons, Ltd.     

Nonlinear pushover analysis of infilled concrete frames

Six reinforced concrete frames with or without masonry infills were constructed and tested under horizontal cyclic loads. All six frames had identical details in which the transverse reinforcement in columns was provided by rectangular hoops that did not meet current ACI specifications for ductile frames. For comparison purposes, the columns in three of these frames were jacketed by carbon-fiber-reinforced-polymer （CFRP） sheets to avoid possible shear failure. A nonlinear pushover analysis, in which the force-deformation relationships of individual elements were developed based on ACI 318, FEMA 356, and Chen＇s model, was carried out for these frames and compared to test results. Both the failure mechanisms and impact of infills on the behaviors of these frames were examined in the study. Conclusions from the present analysis provide structural engineers with valuable information for evaluation and design of infilled concrete frame building structures.