闽北东坑火山盆地白垩纪火山—侵入杂岩的岩石成因与金成矿

火山岩和侵入岩是许多浅成低温热液型金矿床成矿物质和流体的重要来源。中生代时期华南陆块经历了强烈的岩浆—热液活动,在中国东南沿海地区形成了大量的火山—侵入杂岩和浅成低温热液金矿。本文选取该区研究程度较低的闽北政和县东坑火山盆地为研究对象,利用岩相学、年代学、全岩地球化学、Sr—Nd—Hf同位素等方法,来探讨该火山盆地中火山岩和侵入岩的成因联系、岩浆演化过程以及它们与盆地内同时期金矿的关系。东坑火山盆地由多种岩性的火山岩和空间上与其密切共生的浅成侵入相花岗斑岩、石英二长斑岩,以及携带暗色微粒包体的花岗岩脉组成。LA- ICP- MS锆石U- Pb定年显示,东坑的火山岩和侵入岩均形成于白垩纪（101. 0±0. 9~97. 3±1. 2 Ma）,其全岩Sr—Nd同位素组成较均一\[n（87Sr）/ n（86Sr）\]i=0. 7085~0. 7104;εNd(t)= -8. 83~ -7. 34,但锆石Hf同位素组成变化范围较大εHf(t)= -14. 0~3. 3。岩石地球化学特征显示,该盆地火山—侵入杂岩为富碱、富钾的准铝—弱过铝质岩石,这些岩石具有连续线性变化的主量元素特征、右倾的稀土配分曲线、弱至中等的Eu负异常（Eu/Eu* =0. 19~0. 83）、较高的氧逸度（lgfO2=-17. 44~-4. 18）以及大离子亲石元素Rb、K、Pb富集,高场强元素Nb、Ta、Ti亏损的特征。综合年代学及岩石地球化学特征,认为东坑火山盆地中的火山—侵入杂岩是在古太平洋板块俯冲后撤的伸展构造背景下,幔源岩浆上涌促使地壳源岩发生重新熔融并与之混合,不断演化,最终侵位于地壳浅表的产物。岩浆的源区组成、结晶分异和高氧逸度条件等共同造就了该盆地及周围同时期金的成矿。     

CPL7及其在中国地球系统模式中的应用前景

中国地球系统模式中普遍存在的耦合器CPL6(美国国家大气研究中心的第六代通量耦合器)在很大程度上限制了模式在高分辨率上的发展,新一代耦合器CPL7并行度的可扩展性更高,能够适应更高分辨率的构型。以CPL7与中国科学院大气物理研究所的第二代格点大气环流模式(the Version 2 Grid-point Atmospheric Model of Institute of Atmospheric Physics,Chinese Academy of Sciences)的耦合为例,概述了其耦合原理,为CPL7与中国其他模式的耦合提供相关的经验。结合国内外模式的发展方向,CPL7耦合器在中国未来几年的地球系统模式的耦合改进中将占有很大的优势地位。     

Advance in Matrix Effect Study of LA‐MC‐ICPMS U‐Pb Dating on U‐Bearing Oxide Minerals

正Objective With the development of analytic technologies,in-situ dating on U-bearing oxide minerals(e.g.,cassiterite,rutile and baddeleyite)has been widely used in geological chronological researches and has attracted remarkable attention to explore evolution of the earth and obtain age information of various geological processes.Matrix effect     

洛阳市城市环境气象监测预报服务研究

利用洛阳市环境监测资料和气象资料,分析了洛阳市污染物浓度的日变化、季节变化、年际变化规律,并分析了污染物浓度与气象因子的关系。在此基础上,通过回归分析预报方法、污染潜势预报方法、CAPPS模式预报方法对洛阳市3种主要污染物的浓度和级别进行了24 h和48 h预测,并建立了气象局与环保部门共享的气象和污染数据库平台,为双方今后的合作奠定了基础。     

一次层状云飞机播云试验的云微物理特征及响应分析

根据2005年3月21日在河南进行的层状云飞机播云试验的探测资料,对人工增雨催化前后层状云的宏微观物理量进行对比分析.结果表明,播云前在4200m高度平飞中观测到的小云粒子数浓度最大值为1.36×108个/m3,相应平均直径在5μm左右;小云粒子数浓度和云液态水含量在催化后均减小,播撒层下方变化较之播撒层变化更加显著;5000m高度小云粒子平均直径由催化前的17.32μm增加到催化后的18.07μm,平均直径明显增大,这些作业前后微观物理量的变化表明了人工催化层状云的物理响应.不同高度飞行具有相似的粒子谱分布.     

Aerosol spectra and new particle formation observed in various seasons in Nanjing

The aerosol number spectrum and gas pollutants were measured and the new particle formation （NPF） events were discussed in Nanjing. The results showed that the size distributions of aerosol number concen- trations exhibited distinct seasonal variations, implying the relations of particle sizes and their sources and sinks. The number concentrations of particles in the nuclei mode （10-30 nm）, Aitken mode （30-100 nm）, accumulation mode （100 -1000 nm） and coarse mode （〉1μm） varied in the order of summer 〉 spring 〉 autumn, summer 〉 autumn 〉 spring, autumn 〉 summer 〉 spring, and spring 〉 autumn 〉summer, re- spectively. The diurnal variation of total aerosol number concentrations showed three peaks in all observed periods, which corresponded to two rush hours and the photochemistry period at noon. In general, the NPF in summer occurred under the conditions of east winds and dominant air masses originating from marine areas with high relative humidity （50%-70%） and strong solar radiations （400 -700 W m-2）. In spring, the NPF were generally accompanied by low relative humidity （14%-30%） and strong solar radiations （400-600 W m-2）. The new particle growth rates （GR） were higher in the summertime in the range of 10- 16 nm h-1. In spring, the GR were 6.8-8.3 nm h-1. Under polluted air conditions, NPF events were seldom captured in autumn in Nanjing. During NPF periods, positive correlations between 10- 30 nm particles and 03 were detected, particularly in spring, indicating that NPF can be attributed to photochemical reactions.     

陇中黄土高原区旱地春小麦产量对干旱胁迫响应的模拟研究

为进一步探明陇中黄土高原区旱地春小麦产量形成对不同干旱胁迫的响应机制,依据甘肃省定西市安定区凤翔镇安家沟村2016—2018年大田控水试验数据以及定西市安定区1971—2018年气象数据,验证农业生产系统模拟(Agricultural production systems simulation,APSIM)模型模拟不同...     

腐殖酸对U（Ⅵ）的吸附性能研究

砂岩型铀矿的形成与腐殖酸存在密切联系,在铀成矿过程中的化学作用受多方面因素的制约。通过静态吸附试验,探讨了影响腐殖酸吸附U(Ⅵ)的因素,考查了pH值、吸附时间、加入量等的影响。结果表明:pH值对腐殖酸的吸附影响较大,当pH值为6时,吸附率达到最大;少量的腐殖酸就能使U(Ⅵ)吸附率达到98.79%,随着腐殖酸加入量的增加吸附率随之增加,最后趋于平衡;吸附在较短的时间内基本达到平衡。在腐殖酸-粘土、腐殖酸-砂岩二元系统中,混合后吸附效果增加,并且随着腐殖酸加入量的增加吸附率也随之增大,在腐殖酸-粘土-砂岩三元系统中,也得到了相似的吸附趋势。     

Sensitivity of penman-monteith reference crop evapotranspiration in Tao’er River Basin of northeastern China

A non-dimensional relative sensitivity coefficient was employed to predict the responses of reference crop evapotranspiration （ET0） to perturbation of four climate variables in Tao＇er River Basin of the northeastern China. Mean monthly ET0 and yearly ET0 from 1961 to 2005 were estimated with the FAO-56 Penman-Monteith Equation. A 45-year historical dataset of average monthly maximum/minimum air temperature, mean air temperature, wind speed, sunshine hours and relative humidity from 15 meteorological stations was used in the analysis. Results show that： 1） Sensitivity coefficients of wind speed, air temperature and sunshine hours were positive except for those of air temperature of Arxan Meteorological Station, while those of relative humidity were all negative. Relative humidity was the most sensitive variable in general for the Tao＇er River Basin, followed by sunshine hours, wind speed and air temperature. 2） Similar to climate variable, monthly sensitivity coefficients exhibit large annual fluctuations. 3） Sensitivity coefficients for four climate variables all showed significant trends in seasonal/yearly series. Also, sensitivity coefficients of air temperature, sunshine hours and wind speed all showed significant trends in spring. 4） Among all sensitivity coefficients, the average yearly sensitivity coefficient of relative humidity was highest throughout the basin and showed largest spatial variability. Longitudinal distribution of sensitivity coefficients for air temperature, relative humidity and sunshine hours was also found, which was similar to the distribution of the three climate variables.     

我国农村饮水安全问题探讨与对策

根据《我国饮水安全与北方缺水地区农业水资源高效利用战略研究》及《全国农村饮水安全现状调查评估》中的调查资料,统计分析了我国农村饮水不安全人口总体分布特征及 不同类型的空间分布特点。按照中部、东部和西部划分,饮水不安全人口在数量上中部多东部少,中部为1.4 亿人,东部为0.7 亿人;在饮水不安全人口占农村总人口比例上,西部多东部少,西部为40%,东部为27%。饮用高氟、苦咸水、污染地表水、污染地下水以及水量缺乏等不同类型的饮水不安全人口分布特点各不相同,高氟水主要在华北地区,在天津饮用高 氟水人口占不安全人口的70%;饮用污染地表水主要分布在淮河以南、青海西藏以东大部分区域。进一步分析讨论了不同饮水安全问题(高氟、高砷、污染水、水量缺乏等) 的成因及影响农村饮水安全的主要因素,最后提出严格防治点源污染、面源污染,加强水源地保护,加 强雨水集蓄利用以及制定应急机制和预案等一系列解决农村饮水安全问题、保障饮水安全的 对策和措施。