亚热带地区田径足球场的设计和养护

根据多年实践经验和现场实验对亚热带地区田径足球场的设计和保养维护做了较为全面的论述。文中涉及到的足球场建设的方法、所用材料及必要的数据、养护的方法等都经过实践的验证 ,具有较强的可操作性。     

浙江省暖冬的特点与汛期降水关系的分析

利用1951年以来的冬季(12月～2月)气温资料，对暖冬年进行划分，发现暖冬年西风带亚洲地区常出现纬向环流，低纬度西太平洋副热带高压偏强，位置偏西，暖冬年份与浙江省进人汛期后的总降水量和台风次数，都有较好关系。     

The South China Sea is not a mini-Atlantic: plate-edge rifting vs intra-plate rifting

The South China Sea, as ‘a non-volcanic passive margin basin’ in the Pacific, has often been considered as a small-scale analogue of the Atlantic. The recent ocean drilling in the northern South China Sea margin found, however, that the Iberian model of non-volcanic rifted margin from the Atlantic does not apply to the South China Sea. In this paper, we review a variety of rifted basins and propose to discriminate two types of rifting basins: plate-edge type such as the South China Sea and intra-plate type like the Atlantic. They not only differ from each other in structure, formation process, lifespan and geographic size, but also occur at different stages of the Wilson cycle. The intra-plate rifting occurred in the Mesozoic and gave rise to large oceans, whereas the plate-edge rifting took place mainly in the mid-Cenozoic, with three-quarters of the basins concentrated in the Western Pacific. As a member of the Western Pacific system of marginal seas, the South China Sea should be studied not in isolation on its origin and evolution, but in a systematic context to include also its neighboring counterparts.     

太平洋副热带经圈环流的研究

太平洋副热带经圈环流是太平洋热带和副热带上层海洋进行热交换的 桥梁,其变化可以影响太平洋热带和副热带之间的热结构,从而影响全球气候。本文简要介 绍有关研究工作并提出了今后需要研究的问题。     

中国亚热带地区植物区系地理成分及其空间格局的数量分析

选择我国亚热带区域76个地区(不包括行政单元)的植物区系调查和研究资料,采用主成分分析 (PCA)、TWINSPAN聚类和样带梯度分析方法,研究了我国亚热带区域植物区系地理成分的构成特征和 各成分之间的关系;各研究区域间植物区系地理成分构成的相关性和空间分异特征;并分析了贯穿我国亚热带区域的东经108.5°～111.5°和北纬29°～31°两条样带的几种区系地理成分的分布梯度。结果表明：①15种区系地理成分可以归为热带成分、温带成分、干旱区成分和东亚中心成分4组;我国亚热带各地区区系地理成分中泛热带和北温带分布的比例最高;干旱区分布诸类比例极小;东亚中心成分的比例突出,特有性强;②样点的PCA排序明显反映了北、中、南亚热带在区系地理成分构成上的差异,但亚热带东西部的差异不明显;③样带分析清晰地反映了热带、温带成分之比的梯度格局;川东鄂西地区特有分布中心的地位和世界分布与特有成分相反的分布格局。     

新疆东准噶尔克拉麦里蛇绿岩地球化学：洋脊俯冲的产物

新疆东准噶尔克拉麦里蛇绿岩中的镁铁质岩兼具有洋中脊玄武岩（MORB）和岛弧拉斑玄武岩（IAB）的特征，岩石地球化学特征表现为轻稀土（LREE）亏损、平坦或略微富集，不同程度地亏损高场强元素（HFSE）而富集大离子亲石元素（LILE），成分上非常相似于受洋脊俯冲影响的Chile Ridse和Cocos Ridse玄武岩。可以认为其可能形成于受洋脊俯冲影响的岛弧或弧前扩张环境。相对较高的εNd（t）（7．2—9．8）、低Nb／Zr、Ta／Yb比值，说明在洋脊俯冲的影响下，其源区可能存在有至少三种组分：弧下地幔、来自消减板片流体和俯冲沉积物、MORB地幔。     

珠江三角洲地区一次强对流天气物理量场的分析

本文对珠江三角洲地区1983年9月24日在副热带高压控制下强对流天气发生的物理量场进行分析，发现这次强对流天气是在有利的环境条件下发生的。指出了这次强对流天气的可能触发条件，对今后预报此类强对流天气有重要意义.     

九连山亚热带常绿阔叶林小流域气候及水文特征分析

森林及其流域是一个复杂的动态自然生态系统,对其降雨、温度、蒸发和径流的长期研究有助于理解系统生态过程的动态变化。根据江西九连山虾公塘气象观测场1975—2015年逐日气象资料及4号水文观测堰2009—2013年小流域逐日径流资料,应用累积距平和小波变换等方法分析九连山亚热带常绿阔叶林气候和小流域径流变化特征及其二者的一致性。结果表明：① 九连山亚热带常绿阔叶林多年平均温度为17.1 ℃,降雨量为1816.3mm,蒸发量为781.6mm,3—10月降雨量约占全年降雨量的82.6%;②多年平均温度在震荡中呈现微弱上升趋势,温度变化倾向率为0.14 ℃/10a;平均降雨量和蒸发量呈现整体下降趋势,变化倾向率分别为-11.81mm/10a和-50.13mm/10a;年均温度、降雨量和蒸发量均存在准14a左右的主要震荡周期;③九连山常绿阔叶林小流域多年平均径流量为1066.2mm,径流系数为0.54;月径流量与降雨量呈显著的线性关系;大雨以上天气时,径流量恢复到降雨前流量水平的持续时间约为12~48h;年内径流量与降雨量存在20d左右的短周期和60d左右的长周期,与蒸发量的震荡格局基本相似,降水量、蒸发量与径流量的震荡周期具有一致性,径流量对年内气候季节变化的响应明显;降水条件是引起径流量变化的主要原因。这些结果表明气候变化对森林小流域径流量的周期性变化有重要影响。     

Magnesium isotope geochemistry of the carbonate-silicate system in subduction zones

The lighter magnesium (Mg) isotopic signatures observed in intraplate basalts are commonly thought to result from deep carbonate recycling, provided that the sharp difference in Mg isotopic composition between surface carbonates and the normal mantle is preserved during plate subduction. However, deep subduction of carbonates and silicates could potentially fractionate Mg isotopes and change their chemical compositions. Subducting silicate rocks that experience metamorphic dehydration lose a small amount of Mg, and preserve the original Mg isotopic signature of their protoliths. When the dehydrated fluids dissolve carbonate minerals, they may evolve into lighter Mg isotopic compositions. The solubility of carbonate minerals in fluids decreases in the order of calcite, aragonite, dolomite, magnesite and siderite, leading to selective and partial dissolution of carbonate minerals along the subduction path. At the island arc depth (70–120 km), the metamorphic fluid dissolves mainly Mg-poor calcites, and thus the fluid has difficulty modifying the Mg isotopic system of the mantle wedge and associated arc basalts. At the greater depth of the back arc system or continental margin (>150 km), the supercritical fluid can dissolve Mg-rich carbonate minerals, and its interaction with the mantle wedge could significantly imprint the light Mg isotopic signature onto the mantle rocks and derivatives. Meanwhile, the carbonate and silicate remaining within the subducting slab could experience elemental and isotopic exchange, during which the silicate can obtain a light Mg isotopic signature and high CaO/Al₂O₃, whereas the carbonates, particularly the Ca-rich limestone, shift Mg isotopes and MgO contents towards higher values. If this isotopic and elemental exchange event occurs widely during crustal subduction, subducted Ca-rich carbonates can partially transform into being Mg-rich, and a portion of recycled silicates (e.g. carbonated eclogites) can have light Mg isotopic composition alongside carbonates. Both serve as the low-δ²⁶Mg endmember recycled back into the deep mantle, but the latter is not related to deep carbonate recycling. Therefore, it is important to determine whether the light Mg isotopic signatures observed in intraplate basalts are linked to deep carbonate recycling, or alternatively, recycling of carbonated eclogites.     

基于遥感和GIS的亚热带山区土地利用/覆盖时空变化研究

在研究区运用遥感解译技术,监测土地利用变化状况,分析土地利用类型空间位置转换的时空变化特征.结果表明：研究区的土地利用类型以林地和草地为主,土地利用程度总体还比较低;研究时段内,土地利用时空变化较缓慢,正处于调整期.