Latest precambrian (Cadomian) zircon ages, Nd isotopic systematics and P-T evolution of granitoid orthogneisses of the Erzgebirge, Saxony and Czech Republic

Single zircons from two orthogneiss complexes, the Grey Gneiss and Red Gneiss, the lowermost tectonic units in the Erzgebirge, were dated. The grey Freiberg Gneiss is of igneous origin and has a ²⁰⁷Pb/²⁰⁶Pb emplacement age of 550±7 Ma. A quartz monzonite from Lauenstein contains idiomorphic zircons with a mean ²⁰⁷Pb/²⁰⁶Pb age of 555±7 Ma as well as xenocrysts ranging in age between 850 and 1910 Ma. Red gneisses from the central Erzgebirge contain complex zircon populations, including numerous xenocrysts up to 2464 Ma in age. The youngest, idiomorphic, zircons in all samples yielded uniform ²⁰⁷Pb/²⁰⁶Pb ages between 550±9 and 554±10 Ma. Nd isotopic data support the interpretation of crustal anatexis for the origin of both units. _Nd(t) values for the grey gneisses are –7.5 and –6.0 respectively, (mean crustal residence ages of 1.7–1.8 Ga). The red gneisses have a wider range in _Nd(t) values from –7.7 to –2.8 (T _DM ages of 1.4–1.8 Ga). The zircon ages document a distinct late Proterozoic phase of granitoid magmatism, similar in age to granitoids in the Lusatian block farther north-east. However, Palaeozoic deformation as well as medium pressure metamorphism ( 8 kbar/600–650° C) are identical in both gneiss units and distinguish these rocks from the Lusatian granitoids. The grey and red gneisses were overthrust by units with abundant high-pressure relicts and a contrasting P-T evolution. Zircon xenocryst and Nd model ages in the range 1000–1700 Ma are similar to those in granitoid rocks of Lusatia and the West-Sudetes, and document a pre-Cadomian basement in parts of east-central Europe that, chronologically, has similarities with the Sveconorwegian domain in the Baltic Shield.     

江西南部鹤仔片麻状花岗岩类Pb-Pb同位素年龄及地质意义

江西南部鹤仔一带的片麻状花岗岩体是在武夷山西南坡江西境内发现的最古老的片麻状花岗岩体.选取晶形好,无磁性锆石进行了Pb-Pb同位素年龄测定,获得片麻状黑云母二长花岗岩体1848±20Ma、1774±20Ma,片麻状花岗闪长岩体为996±29Ma.它对进一步认识该区"中条"至"晋宁"期岩浆活动构造背景,中深变质岩时代确定等具有一定的意义.     

皖浙赣相邻区中元古代溪口岩群的划分与对比

通过1：25万区调工作，对变质岩区采用了构造一地(岩)层法填图，区域性标志层的追索与对比，以及所获得的同位素年龄成果，对研究区长期存在的同物异名及同名异物的现象得到了较好的理顺。根据溪口岩群的岩石组合、沉积构造、变质变形特征，将其划分为佛子坑、板桥、木坑、郑家坞四个岩组。溪口岩群和双桥山群、双溪坞群应属大致同时、但在不同大地构造背景下不同沉积环境的产物，溪口岩群与双桥山群、双溪坞群层位相当，但岩性组合差异较大。     

不同城市PM2.5对易感小鼠线粒体损伤的影响

采集太原市冬季大气细颗粒物（PM_2.5）,选取4周、4月、10月龄C57BL/6雌性小鼠,采用咽后壁滴注的方法用3mg/kg（体重）PM_2.5暴露4周.此外,分别采集太原市、北京市、杭州市和广州市4个城市的冬季PM_2.5,将10月龄小鼠暴露其中.采用荧光定量PCR技术检测心脏组织中细胞色素C氧化酶亚基I（co1）、IV（co4）和ATP合酶（ATP6）以及核转录因子pgc-1α、nrf1和tfam的mRNA转录水平.结果发现,太原市PM_2.5暴露后,10月龄小鼠心脏组织中co1、co4和ATP6以及核转录因子pgc-1α、nrf1和tfam的mRNA水平与对照组相比均显著升高.但4周和4月龄小鼠中上述基因表达则未见明显差异.10月龄小鼠暴露于不同城市PM_2.5后,杭州PM_2.5暴露可引起小鼠心脏组织中co1、co4、ATP6、pgc-1α、tfam的mRNA表达上升.北京PM_2.5暴露可引起小鼠心脏组织中co1、ATP6和tfam的mRNA表达显著上升;广州PM_2.5暴露则未见上述任何基因表达的显著改变.研究表明,太原市PM_2.5对易感小鼠心脏线粒体氧化磷酸化的影响最大,其次是杭州市和北京市,而广州市的影响最小.     

植茶年限对土壤酸度及其团聚体交换性酸分布的影响

为明晰土壤酸度与团聚体交换性酸对植茶年限的响应特征,采用野外实地调查和室内分析相结合的方法,以植茶16、23、31和53 a的土壤为研究对象,开展不同植茶年限对土壤酸度及其团聚体交换性酸分布的影响.结果表明:①随着植茶年限的延长,土壤pH逐渐降低,交换性氢、交换性铝和交换性酸含量均呈升高的趋势.各植茶年限土壤0~20 cm土层pH均低于>20~40 cm土层,而交换性氢、交换性铝和交换性酸含量则表现出相反的变化趋势,且交换性氢含量在植茶23 a后的增幅可达21.29%. ②土壤交换性氢、交换性铝和交换性酸含量均随团聚体粒径的减小而升高,各粒径团聚体交换性氢、交换性铝和交换性酸含量随植茶年限的延长而逐渐升高. ③各植茶年限土壤团聚体交换性氢的分配比例均远低于交换性铝.随团聚体粒径的减小,各植茶年限交换性氢的分配比例均呈升高的趋势,而交换性铝的分配比例则呈降低趋势. 0~20 cm土层各粒径团聚体交换性氢的分配比例均以植茶53 a时较高,为17.97%~19.69%;>20~40 cm土层各粒径团聚体交换性氢的分配比例以植茶16 a时较高,为19.51%~22.77%,而各粒径团聚体交换性铝的分配比例则呈相反的趋势.研究显示,长期植茶会导致土壤酸化,随着植茶年限的延长,土壤pH逐渐降低,交换性氢、交换性铝和交换性酸含量均升高,不同粒径团聚体对交换性酸的保持能力存在明显差异.      

黄土丘陵区林草退耕年限对土壤团聚体特征的影响

随着国家退耕还林还草战略的实施、植被覆盖的变化,林、草地植被恢复进程中土壤团聚体特征的变化受到广泛关注.本研究以黄土丘陵区西部的官山林场退耕后栽植的刺槐林地、撂荒草地为对象,选取退耕年限为10、25 a的林、草地,采用湿筛法测定各样地0~30 cm土壤的水稳性团聚体组成,比较退耕还林、还草和退耕年限(10、25 a)对土壤水稳性团聚体平均质量直径(MWD)和分形维数(D)的影响.结果表明:退耕10 a的林地0~30 cm土层水稳性大团聚体含量(R0.25)、MWD和D分别为57.60%、1.91 mm和2.73;退耕25 a的林地分别为60.17%、1.88 mm和2.74;退耕10 a的草地分别为59.89%、1.82 mm和2.74;退耕25 a的草地分别为72.69%、2.71 mm和2.61.进一步分析证明,随着退耕年限的增加,土壤团聚性增强;但林草地的变化存在差异:恢复10 a阶段,土壤团聚性林地尚优于草地,25 a后草地优于林地.各样地土壤的SOC含量与R0.25呈显著正相关关系(p0.01),与D呈显著负相关关系(p0.05).退耕类型和退耕年限对土壤团聚性有显著影响.     

滨海滩涂围垦区不同围垦年限土壤酶活性变化及其与理化性质关系

土壤酶几乎参与所有的土壤生物化学过程,厘清土壤酶活性与土壤理化性质的关系能够揭示围垦后土壤质量变化状况,为土壤生态系统的科学调控提供理论依据.选择江苏中部如东不同围垦年限(7、32、40、63 a)的滩涂围垦区为研究对象,以未围垦光滩作为对照(0 a),利用经典统计学分析和冗余分析研究不同围垦年限土壤酶活性变化过程,及其与土壤理化性质之间的关系.经典统计学分析表明不同围垦年限间土壤酶活性具有显著性差异,淀粉酶、脱氢酶和酸性磷酸酶活性随着围垦年限的增长呈现出先上升后下降的过程,而脲酶和碱性磷酸酶活性则随着围垦年限的增长呈现出先上升-下降-再上升的过程.同时,不同围垦年限的表层土壤酶活性基本上高于深层.冗余分析表明5种理化性质在前两轴累积能够解释土壤酶活性的69.8%,pH、电导率、土壤有机碳、全氮和全磷与土壤酶活性呈极显著相关关系(P0.01).土壤理化性质对土壤酶活性影响重要性大小排序为全氮有机碳pH全磷电导率.     

Characterization of refuse landfill leachates of three di erent stages in landfill stabilization process

Landfill leachates with di erent ages (mature leachate, 11 years; semi-mature leachate, 5 years; fresh leachate, under operation) were collected from Laogang Refuse Landfill, Shanghai to characterize the colloid size distribution and variations of leachate. These leachates were separated using micro-filtration and ultra-filtration into specific size fractions, i.e., suspended particles (SP) (> 1.2 m), coarse colloids (CC) (1.2–0.45 m), fine colloids (FC) (0.45 m, 5 kDa/1 kDa molecular weight (MW)), and dissolved organic matters (DM, < 5 kDa/1 kDa MW). The specific colloids in each size fraction were quantified and characterized through chemical oxygen demands (COD), total solid (TS), pH, NH4 +-N, total organic carbon (TOC) and fixed solid (FS). It was found that COD, NH4 +-N and TS in leachate decreased significantly over ages, while pH increased. The dissolved fractions (< 5 kDa/1 kDa) dominated (over 50%) in three leachates in terms of COD, and the organic matter content in dissolved fraction of leachates decreased and the inorganic matter increased as the disposal time extended, with the TOC/COD ratio 30%–7%. Dissolved fractions decreased from 82% to 40% in terms of TOC as the disposal time extended, suggested that the organic matter remained in leachate would form into middle molecular weight substances during the degradation process.     

Characterization of refuse landfill leachates of three different stages in landfill stabilization process

hate would formed into middle molecular weight substances during the degradation process.     

中国机动车行驶里程分布规律

机动车行驶里程是计算机动车尾气排放量的一个重要参数.对全国数百个地级及以上城市不同车龄的机动车(包括轻型客车、公交车、出租车和摩托车)行驶里程进行了调查.结果表明:除公交车外,其他机动车的累积行驶里程均随车龄而呈现对数递减性,即车龄越长机动车的累积行驶里程增加越慢,年使用率越小;某类型机动车车队的年均行驶里程与调查基准年的各车龄机动车的保有量相关;提出了轻型客车年行驶里程和车龄的经验公式,并得到2007年轻型客车的年均行驶里程为2.691×104km.