A SENSITIVE AUTOMATED METHOD FOR DETERMINATION OF MERCURY IN GEOLOGICAL MATERIALS BY COLD VAPOR ATOMIC ABSORPTION

An improved sensitive automated method for the determination of mercury in geological materials by cold vapor atomic absorption has been developed. Sample is digested with nitric and hydrochloric acids at low heat. Mercuric ions in the digested sample solution are reduced to elemental mercury by stannous chloride. The gaseous mercury separated from the solution is swept by a stream of argon into the absorption cell of an LDC/Milton Roy Mercury Monitor where the atomic absorption at 253.7 nm is measured. The precision of the method is 2.7% r.s.d., and the detection limit is 1 ppb. The results on 53 international geochemical reference samples are presented.     

海洋解木糖赖氨酸芽孢杆菌JZ008对重金属Cd2+、Cr3+和Cu2+的吸附作用

利用单因素实验对海洋解木糖赖氨酸芽孢杆菌(Lysinibacillus xylanilyticus sp.JZ008)培养条件进行了优化.优化后的培养条件:温度为35℃、pH值为7.5、接种量为3%(V/V)、装液量为50cm3/250 cm3时,菌量达到2.01×108CFU/cm3,比优化之前提高了40.6%.添加海藻寡糖可以促进菌株生长,添加量为5.0 g/dm3时发酵液中活菌数是对照组的2.51倍.研究了菌株JZ008对Cd~(2+)、Cr~(3+)、Cu~(2+)3种重金属离子的吸附特性,结果表明菌株JZ008对3种重金属离子污染的水溶液吸附率效果明显,20 d吸附率分别达到95.6%、96.4%、87.0%.土壤重金属吸附实验结果表明,海藻寡糖复配菌株JZ008组对Cd~(2+)、Cr~(3+)、Cu~(2+)吸附效果明显,60 d吸附率分别达到82.5%、82.0%、86.9%.菌株JZ008对重金属的优良吸附作用为进一步开发解木糖赖氨酸芽孢杆菌在重金属修复方面的应用奠定了基础.     

韩国济洲岛下西归浦组的时代及其古环境

韩国济洲岛下西归浦组的时代归属一直存在着争论。该段地层中浮游有孔虫 Globigerina calida calida、Beella digitata、 Globigerina bermudezi和 Globoquadrina conglomerata的发现表明了它应为中更新世 (晚 N 2 2带、即 Globigerina calida calida亚带 ,不晚于 40万年前 )的沉积。底栖、浮游有孔虫的定量统计分析揭示了下西归浦组沉积环境的变化 :下部的沉积环境为岸外中陆架暖水 ,而向上则演变成近岸内陆架温凉水。有孔虫组合的更替反映了下西归浦组沉积是一个由次一级的 3个亚海退和 2个亚海进组成的海退序列。     

Spatio-temporal variability in sea surface wind stress near and off the east coast of Korea

Sea surface wind stress variabilities near and off the east coast of Korea, are examined using 7 kinds of wind datasets from measurements at 2 coastal (land) stations and 2 ocean buoys,satellite scatterometer (QuikSCAT), and global reanalyzed products (ECMWF,NOGAPS,and NCEP/NCAR). Temporal variabilities are analyzed at 3 frequency bands; synoptic (2-20 d), intra-seasonal (20-90 d),and seasonal (>90 d).Synoptic and intra-seasonal     

剧毒卡尔藻与东海原甲藻间的化感作用研究

为研究剧毒卡尔藻(Karlodinium veneficum)与东海原甲藻(Prorocentrum donghaiense)之间的化感作用,在f/2营养盐条件下,分别采用了混合培养及滤液培养的方法。结果表明:剧毒卡尔藻指数生长后期的无藻细胞滤液明显抑制了东海原甲藻的生长,而东海原甲藻滤液对剧毒卡尔藻的生长几乎无影响,化感作用作为重要的影响因素使剧毒卡尔藻获得竞争优势。将剧毒卡尔藻指数生长末期的无藻细胞滤液置于固相萃取(SPE) C18小柱,经吸附、不同比例的甲醇溶液洗脱,考察不同洗脱部分对东海原甲藻生长的影响,发现80%的甲醇洗脱部分明显抑制了东海原甲藻的生长。本研究为了解剧毒卡尔藻的竞争机制提供了重要的科学依据,今后将重点分析剧毒卡尔藻释放的有效抑制东海原甲藻生长的化感物质。     

在特殊疫情背景下《城市地理资讯学》MOOC课程教学实施效果分析

在新冠肺炎疫情期间,线上教学大规模开展,相关线上教学问题逐渐成为研究热点。传统的测绘地理类课程的教学方式主要是上课时以老师传授知识为主,课后以学生完成作业为辅的方式进行。但是,这种教学方式比较单一,并且在科学化考核和促进学生学习主动性等方面存在诸多问题。然而,线上网络课程是通过互联网以电子设备为教学平台,具有不受教学时空限制、教学方法灵活多样和丰富学生的学习方式等优点。因此,对《城市地理资讯学》MOOC(massive online open courses)课程实施效果进行分析,为其他测绘地理类网络课程设计提供优化思路,同时为无法进行面授教学的特殊时期提供一种有效的教学方案。     

NUMERICAL SIMULATION ON THE WIND FIELD STRUCTURE OF A MOUNTAINOUS AREA BESIDE SOUTH CHINA SEA DURING THE LANDFALL OF TYPHOON MOLAVE

Leveraging the commercial CFD software FLUENT, the fine-scale three-dimensional wind structure over the Paiya Mountains on the Dapeng Peninsula near Shenzhen, a city on the seashore of South China Sea, during the landfall of Typhoon Molave has been simulated and analyzed. Through the study, a conceptual wind structure model for mountainous areas under strong wind condition is established and the following conclusions are obtained as follows： （1） FLUENT can reasonably simulate a three-dimensional wind structure over mountainous areas under strong wind conditions; （2） the kinetic effect of a mountain can intensify wind speed in the windward side of the mountain and the area over the mountain peak; and （3） in the leeward side of the mountain, wind speed is relatively lower with relatively stronger wind shear and turbulence.     

The impact of cumulus parameterizations and microphysics schemes under different combinations on typhoon track prediction

This study examines the effects of cumulus parameterizations and microphysics schemes on the track forecast of typhoon Nabi using the Weather Research Forecast model. The study found that the effects of cumulus parameterizations on typhoon track forecast were comparatively strong and the typhoon track forecast of Kain-Fritsch (KF) was superior to that of Betts-Miller (BM). When KF was selected, the simulated results would be improved if microphysics schemes were selected than otherwise. The results from Ferrier, WSM6, and Lin were very close to those in the best track. KF performed well with the simulations of the western extension and eastern contraction changes of a North Pacific high as well as the distribution and strength of the typhoon wind field.     

Fault tectonic analysis of Kii peninsula,Southwest Japan: Preliminary approach to Neogene paleostress sequence near the Nankai subduction zone

The southern part of the Outer Zone of Southwest Japan including the Kii peninsula belongs to the tectonic ‘shadow zone’, where fewer conspicuous active faults and less Quaternary sediments develop than in the Nankai subduction zone and Inner Zone of Southwest Japan. In order to study the paleostress sequence of the Kii peninsula, we analyzed fault‐slip data and tension gashes at pilot sites of Early–Middle Miocene forearc sediments and Late Cretaceous accretionary complex. According to the results, six faulting events are reconstructed in sequence: (i) east–west extension (normal faulting); (ii) east–west compression and north–south extension (strike‐slip faulting); (iii) NNW–SSE compression and ENE–WSW extension (strike‐slip faulting); (iv) northeast–southwest compression and northwest–southeast extension (strike‐slip faulting); (v) WNW–ESE compression (strike‐slip or reverse faulting); and (vi) NNE–SSW extension. The north–south to NNW–SSE trending dyke swarm of Middle Miocene age in the Kii peninsula is thought to be related to Event 3, implying that Event 3 was active at least during the Middle Miocene. Because Event 6 is recognized solely at a site, the overall latest faulting event seems to be Event 5. Assuming that the compression results from the motion of the crust or plate, the compression direction of Event 5 is in good accordance with the present‐day WNW crustal velocity vectors of the Kii peninsula. The stress trajectory map of Southeast Korea and Southwest Japan reveals that the current compression directions of the Kii peninsula correspond to the combinatory stress fields of the Himalayan and Philippine Sea tectonic domains.