Discovery of High-Pressure Basic Granulite Terrain in North China Archaean Craton and Preliminary Study

High-pressure basic granulite terrain of 2.65 Ga from Jiouhuai'an in the junction of the Hebei and Shanxi provinces was discovered and reported recently. The three metamorphic mineral assemblages and their mineral reaction texture of the basic granulites have been identified, which represent three main metamorphic episodes of 1.4—1.5 Gpa, 800℃; 0.7—0.9 Gpa, 820℃ and 0.5—0.6 Gpa, 700℃. Their steep decompressional clockwise P-T path implies that a late Archaean continental collision and sole thrusting event perhaps occurred in North China Craton. This is important to study petrogenesis of high-pressure granulites, composition and texture of deep crust in North China Craton, and early Precambrian collision tectonism.     

地下强爆炸诱发地表塌陷的试验模拟与应用

地下核爆炸后会在地表产生下陷弹坑、塌陷带等不可逆变形爆炸后效应,利用地表形变信息对地下核试验进行有效监控和评估具有十分重要的意义。基于考虑重力影响的地下强爆炸塌陷成坑相似理论,利用陆军工程大学自主研制的地下爆炸效应真空室模拟试验装置,对2017年9月3日朝鲜地下核试验诱发的地表不可逆变形进行了模型试验。试验结果表明,地表塌陷带半径为257 m,下陷弹坑的半径为154 m,与美国、前苏联等国家已有的地下核试验经验公式的数据结果基本相当,并且符合天基雷达TS-InSar卫星监测数据的估算结果,验证了地下爆炸真空室模型试验在地下强爆炸诱发地表不可逆变形区域模拟和评估的可行性,成为有效补充地震波和卫星监测地下强爆炸的一种研究手段。     

广西车田红辉沸石对不同离子吸附性的初步研究

研究表明，不同粒度的红辉沸石在不同的温度条件下对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 等离子具有不同的吸附容量。在30℃时，8μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.90mg/g、10.01mg/g、7.64mg/g、5.50mg/g、108.70mmol/100g；45μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.10mg/g、9.80mg/g、6.90mg/g、5.08mg/g、101.10mmol/100g；246μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：2.66mg/g、2.20mg/g、1.86mg/g、1.26mg/g、28.00mmol/100g；在2℃时，8μm的红辉沸石对K^ 、Na^ 、Ca^2 、Mg^2 、NH4^ 的吸附量分别为：10.60mg/g、9.82mg/g、6.90mg/g、5.07mg/g、99.60mmol/100g。在常温25－30℃，湿度82％条件下，246μm、45μm、8μm的红辉沸石含水率为7.06%、7.25%、7.78%。     

Distribution pattern of artificial radionuclides in the Baltic Sea in the special event of the Chernobyl fallout

Extensive investigations on radioactive contamination and on its spatial and temporal changes in the Baltic Sea have been carried out by the National Board for Atomic Safety and Radiation Protection since 1986. The results were compared with data obtained in the years prior to the Chernobyl accident. Due to the composition of the accidental releases and the physical half-life of the released radionuclides, special emphasis was laid on Cs-134 and Cs-137. Other radionuclides, such as H-3, Sr-90, Ru-103 and Ru-106 turned out to be insignificant compared with the caesium isotopes. The radionuclides Cs-134 and Cs-137 accounting for the highest percentage of the released long-lived radionuclides were deposited on the sea surface with an initial ratio of 0.5. Their distribution pattern on the sea surface was affected by the meteorological conditions prevailing during the release period. The horizontal dislocation of higher contaminated water masses and the vertical penetration of radioactive caesium resulted in a prolonged uniformity of the contamination level of the Baltic Sea.     

Hydrology of the North Klondike River: carbon export,water balance and inter-annual climate influences within a sub-alpine permafrost catchment

Arctic and sub-arctic watersheds are undergoing significant changes due to recent climate warming and degrading permafrost, engendering enhanced monitoring of arctic rivers. Smaller catchments provide understanding of discharge, solute flux and groundwater recharge at the process level that contributes to an understanding of how larger arctic watersheds are responding to climate change. The North Klondike River, located in west central Yukon, is a sub-alpine permafrost catchment, which maintains an active hydrological monitoring station with a record of >40 years. In addition to being able to monitor intra-annual variability, this data set allows for more complex analysis of streamflow records. Streamflow data, geochemistry and stable isotope data for 2014 show a groundwater-dominated system, predominantly recharged during periods of snowmelt. Radiocarbon is shown to be a valuable tracer of soil zone recharge processes and carbon sources. Winter groundwater baseflow contributes 20?% of total annual discharge, and accounts for up to 50?% of total river discharge during the spring and summer months. Although total stream discharge remains unchanged, mean annual groundwater baseflow has increased over the 40-year monitoring period. Wavelet analysis reveals a catchment that responds to El Niño and longer solar cycles, as well as climatic shifts such as the Pacific Decadal Oscillation.

Dedicated to Professor Peter Fritz on the occasion of his 80th birthday     

汝阳地区熊耳群火山岩内夹层硅质岩的微区特征及地质意义

熊耳群是前寒武纪火山-沉积作用的产物,其顶部的马家河组(玄武)安山质火山岩内发育了夹层状热水成因硅质岩。选择熊耳群马家河组硅质岩夹层中的碧玉岩为对象,利用偏光显微镜,XRD,Raman和EBSD等方法剖析了其微区特征。研究结果显示：硅质岩内石英颗粒的显微镜和EBSD照片均表现出颗粒细小、结晶程度低和紧密堆积结构等特点,这完全吻合热水沉积硅质岩的特征;硅质岩内粒径不同的颗粒呈条带(或薄层)状交互出现,不同条带(或薄层)内矿物的组成存在明显的差异,这应该反映了原始物质供给的周期性变化;XRD分析结果指示硅质岩内的主要矿物为低温石英,其晶胞参数为a=b=0.491 3 nm,c=0.540 5 nm和Z=3;EBSD照片和Raman分析结果显示硅质岩内微量的杂质矿物形成于不同阶段,其中粘土矿物和黄铁矿呈零星分布并反映了原始沉积成因,长英质矿物和铁镁硅酸盐矿物均来源于火山凝灰质沉积;火山凝灰质矿物的颗粒偏大并构成了硅质岩内的粗颗粒条带(或薄层),它们与热水沉积为主的细颗粒矿物条带(或薄层)交互产出,这反映了火山作用的周期性反复活动;后期的碳酸盐热液沉淀于硅质岩内裂隙中,它们还导致石英颗粒边缘有序度升高。虽然熊耳群硅质岩内的矿物种类和成因均极为复杂,但火山物质的输入是导致熊耳群硅质岩SiO₂含量偏低的根本原因并得到了硅质岩内大量火山成因矿物的证实。在硅质岩的微组构研究中,Raman光谱分析可以有效的揭示微区上矿物的类型、微区结构及有序度,这些特征是反映硅质岩内部矿物形成与演化过程中微区变化的重要信息。     

基于XRD-Rietveld全谱拟合技术定量分析花岗岩风化壳中矿物组成

XRD-Rietveld全谱拟合方法突破了传统XRD定量分析的众多技术局限,在解决复杂多相混合物的定量问题方面具有显著优势。将XRD-Rietveld全谱拟合方法引入风化壳矿物学研究,有助于解决长期以来地学界对风化壳中矿物组分缺乏准确定量认知的技术瓶颈。在制定专门针对风化样品的全谱拟合精修策略基础上,以广西玉林大容山地区的花岗岩风化壳为研究对象,对发育在两组不同岩性之上的风化剖面(剖面A和剖面B)进行了对比研究。结果表明,风化剖面A(母岩为粗粒黑云母花岗岩)的矿物组合及含量变化范围为：高岭石(6.05%～44.67%)+伊利石(15.85%～49.59%)+石英(29.72%～46.15%)+钾长石(12.04%～22.85%)+斜长石(24.33%～32.70%);风化剖面B(母岩为细粒黑云母花岗岩)的矿物组合及含量变化范围为：高岭石(3.12%～11.47%)+伊利石(13.95%～31.94%)+石英(26.60%～58.05%)+钾长石(13.70%～43.47%)+斜长石(17.95%～23.47%)。两组剖面的全谱拟合修正因子R_wp值<15且gof值<5,计算谱与原始谱拟合效果好,指示矿物定量数据可靠,且能与地质规律较好匹配。在地质意义上,本研究通过母岩原生矿物与次生矿物的含量同步变化,深入揭示了研究区内花岗岩的化学风化过程,厘定了长石类矿物在亚热带气候环境下所经历的长石→伊利石→高岭石演变序列。基于剖面A与剖面B中粘土矿物总量和矿物构成出现显著差异,研究认为在研究区内粗粒黑云母花岗岩比细粒黑云母花岗岩更易遭受强烈的化学风化作用。     

不同耐热型春玉米品种对高温的光谱特征响应

运用两种光谱仪（SPAD-502叶绿素仪与Sunscan植物冠层分析仪）分析了华北平原不同耐热型春玉米品种的光合性能对灌浆期高温的光谱学特征响应。田间试验于2011年—2012年在河北省吴桥县进行。品种选用天玉198、兴玉998与天润606,设置2个播种期（4月15日与4月25日）,于灌浆期测定3个光谱特征值,即叶绿素相对含量（SPAD）、叶面积指数（leaf area index, LAI）与光合有效辐射（photosynthetically active radiation, PAR）。结果表明,播种期4月15日与4月25日相比,春玉米灌浆期≥33 ℃日最高气温的天数与日均温分别增加了3.5 d和0.8 ℃,而日照时数、降雨量、气温日较差及生育期长短均相似; 天玉198与兴玉998、天润606相比,耐热指数（stress tolerance indices, STI）分别高2.9%,11.0%; 根据STI由大到小的顺序,将天玉198、兴玉998与天润606分别定为耐热型、较耐热型与不耐热型品种; 播种期4月15日,天玉198比兴玉998、天润606的产量分别高4.1%,13.7%,SPAD分别高12.5%,19.6%,LAI分别高5.3%,5.6%,PAR分别高4.0%,14.0%; 播种期4月25日,产量分别高1.3%,2.8%; SPAD分别高3.5%,6.0%,LAI分别高1.7%,4.1%,PAR分别高-4.4%,0.9%; 三个品种在高温胁迫环境下产量差异显著,耐热型品种具有显著的产量、SPAD与LAI优势（p＜0.05）。播种期4月15日相对于4月25日,天玉198、兴玉998、天润606的产量分别降低了3.2%,5.9%,12.6%; SPAD分别降低了8.6%,12.4%,15.7%; LAI分别降低了11.7%,17.6%,19.8%; PAR分别降低了3.4%,11.3%,14.5%; STI与SPAD的降幅（r=-0.883,p＜0.05）、LAI的降幅（r=-0.853,p＜0.05）均呈显著负相关,与PAR的降幅（r=-0.923,p＜0.01）呈极显著负相关; SPAD的降幅与PAR的降幅（r=0.872,p＜0.05）呈显著正相关; LAI的降幅与PAR的降幅（r=0.943,p＜0.05）呈极显著正相关。综上所述,耐热型春玉米品种在灌浆期受高温胁迫时,能够在个体层面保持相对较高的叶绿素含量,在群体层面保持相对较高的叶面积,进而保持了较高的光能截获与利用,削弱了高温对光合的抑制程度,缩小了产量降幅,实现了高产与稳产; 品种的耐热性可以通过其光谱特征（SPAD,LAI和PAR）对高温的响应作为鉴定与评价的主要指标之一,为利用光谱特征研究玉米耐热性提供了依据。     

Heavy Metal Ions Determination in the Arctic Soils

ABSTRACT

Soil samples collected in the following areas: Greenland, Svalbard and North Siberia have been analyzed. Seventeen micro and trace elements were determined by ICP-AES.     

石墨炉原子吸收光谱法测定 北美自然铜矿中的铅

采用石墨炉原子吸收光谱法对北美多个自然铜矿区的55个样品进行了铅含量分析,在制作校准曲线时加入高纯铜溶液以消除基体效应影响,高纯铜及样品加标回收率分别为104.0%和111.0%,表明该方法具有较高的可信度.分析结果表明,北美自然铜中铅含量极低,多数含量低于1μg/g,少数介于1-10μg/g之间.