A wind tunnel study of aeolian sand transport on a wetted sand surface using sands from tropical humid coastal southern China     

Qingjie Han  Jianjun Qu  Kongtai Liao  Shujuan Zhu  Kecun Zhang  Ruiping Zu  Qinghe Niu 《Environmental Earth Sciences》2011,64(5):1375-1385

This article reported a wind tunnel test of sediment transport related to surface moisture content and wind velocity using sands from tropical humid coastal area. A 1 mm-thick portion of surface sand was scraped using a self-made sediment sampler, and the gravimetric moisture content was determined. Sand transport was measured via a standard vertical sand trap with a 60 cm height. The result shows that the sand transport profile above the wet surface can be expressed with an exponential equation. In general, the influence of moisture content on sand transport profile mainly focuses on the bottom of the blowing sand cloud. Meanwhile, with moisture content increased, total sand transport dropped, and a relatively larger proportion is transported at greater heights. The vertical movement of particles on higher moisture surface (0.587% < M < 1.448%) is more sensitive to moisture content variation as compared to those on low wet surface (M < 0.587%), total sand transport rate tends to be rather low (0.99 g cm⁻¹ s⁻¹) when M > 1.448%. The total sand transport rate varying with moisture content is divided into three regions of differing gradient at the moisture contents of 0.587 and 1.448%. The gradient of the curve reflected the different influences of the various water forms in surface sediments. The higher moisture surface (M > 1.448%) merely functions as a transport plain for the saltation material. Surface moisture content was the dominant control factor for saltation activity between the moisture contents of 0.587 and 1.448%, wind velocity could resume control saltation after the surface dried to the extent (M < 0.587%).  相似文献   

新型PTH-Ⅵ型气象参数测量仪的研制     

欧同庚  项大鹏  邓涛  廖成旺 《大地测量与地球动力学》2011,31(Z1):165-167

介绍一种新型气象参数测量仪的主要技术指标和功能特点.该仪器使用了高准确度的HD9008TR温湿度传感器、MS5534C气压传感器,采用先进的电子线路设计,具有准确度高、稳定性好、可扩展性强、性能价格比高等特点,满足常规气象监测.  相似文献   

新疆卡拉麦里上-中泥盆统间角度不整合和346.8 Ma后碰撞火山岩的意义   总被引：2，自引：0，他引：2       下载免费PDF全文

王富明  廖群安  樊光明  程雯娟  田健  陈帅  吴魏伟  胡朝斌 《地球科学》2014,39(9):1243-1257

在东准噶尔卡拉麦里地区的五彩湾一带出露一套具磨拉石特征的火山沉积建造, 下部为具磨拉石特征的砾岩、砂岩, 上部为一套中基性的火山熔岩夹中酸性的火山凝灰岩.1:20万卡拉麦里山幅将其归入下石炭统松喀尔苏组.通过1:5万地质调查研究发现, 该火山沉积建造底部以一套粗砾岩高角度不整合于下-中泥盆统卡拉麦里组之上, 含晚泥盆世植物化石Prelepidodendron sp.(先鳞木), 中上部火山岩LA-ICP-MS锆石U-Pb年龄为346.8±3.3 Ma, 且被年龄为341.1±4.0 Ma~340.9±5.1 Ma后碰撞花岗岩侵入, 表明其形成时代为晚泥盆世-早石炭世, 时代上对应于北准噶尔地层分区的上泥盆统克安库都克组.该套地层中上部的火山岩的岩石组合为玄武岩、玄武安山岩、夹少量的流纹质凝灰岩, 岩石化学特征上属钙碱性-高钾钙碱性系列, (La/Yb)_N=2.97~6.66, Nb、Ta亏损, 部分样品Zr、Ti弱显亏损, Nb/U、Ce/Pb比值分别为7.43~20.88、3.17~12.45.地球化学特征表明其兼具板内火山岩和弧火山岩的某些特点, 形成于后碰撞伸展环境, 是卡拉麦里洋盆于晚泥盆世之前闭合后后碰撞岩浆活动的产物.这一研究成果对广为关注的卡拉麦里洋盆的闭合时间进行了很好的限定.   相似文献   

Treatment of Cr(VI) contaminated water with Pannonibacter phragmitetus BB     

Yangyang Wang  Bing Peng  Zhihui Yang  Chongjian Tang  Yuehui Chen  Qi Liao  Yingping Liao 《Environmental Earth Sciences》2014,71(10):4333-4339

Pannonibacter phragmitetus BB was utilized to treat hexavalent chromium [Cr(VI)] contaminated water. Cr(VI) concentration of the contaminated water (pH 10.85) was 534 mg/L. With the inoculum size ranging from 1 to 20 %, P. phragmitetus BB completely reduced Cr(VI) within 27 h when the initial medium concentration exceeded 20 g/L. The lag time of bio-reduction by Cr(VI)-induced cells was 24 h, which was longer than the non-Cr(VI)-induced cells. Under the agitation condition, an obvious bio-reduction lag phase existed and Cr(VI) was completely reduced within 24 h. However, the lag phase was not observed under the static condition, Cr(VI) was reduced continuously after inoculation and Cr(VI) was completely reduced after 27 h incubation. The main chromium components after Cr(VI) reduction were Cr(OH)₃, Cr₂O₃ and CrCl₃. The results of this study are fundamentally significant to the application of P. phragmitetus BB in the treatment of Cr(VI) contaminated water.  相似文献   

广东省市际边界城镇发展的空间类型划分     

廖开怀  陈姝卉 《热带地理》2022,42(3):431-443

利用中国县域统计年鉴（乡镇卷）和中国GDP空间分布公里网格数据集等各类数据,采用因子分析、莫兰指数和GIS分组分析法,对广东省市际边界城镇发展的空间类型进行定量的实证研究。结果表明,广东省市际边界城镇空间结构由公共服务设施与旅游资源类、企业与人口集聚类、生态本底资源类、人民生活水平类以及边缘艰苦类5个主成分因子构成,不同主因子的空间关联性存在差异,其中生态本底资源类和企业与人口集聚类主因子的空间关联性最强,而边缘艰苦类主因子的空间关联性最弱。市际边界城镇的空间发展类型可以划分为高生活水平型发展强镇、产业与人口集聚型发展强镇、产业与公服配套型发展强镇、公服滞后型发展强镇、生态发展型一般镇、生态与旅游型发展一般镇、边缘山区型发展弱镇7类。自然资源禀赋与区位、社会经济发展水平和产业结构、历史基础、政府政策和文化差异为影响市际边界城镇发展空间类型的5大因素。  相似文献   

The spatial pattern and governance of Zhongyuan Urban-Rural System in its development trajectory     

Fu  Haiyue  Wang  Yan  Mao  Liang  Hong  Nana  Wang  Zhaoya  Zhao  Shuchang  Liao  Chuan 《地理学报(英文版)》2022,32(7):1261-1280

Journal of Geographical Sciences - It remains unclear on how transportation network interacts with economic network in an urban-rural agglomeration, while such knowledge is crucial for urban-rural...  相似文献   

拉萨地体中部古新世早期灯垌火山-侵入杂岩成因及地壳硅质岩浆演化          下载免费PDF全文

周逍遥  张玉修  张吉衡  胡俊成  李武毅  黄荣才  廖驾  王家浩  唐显春  朱利东 《地球科学》2021,46(2):474-488

花岗岩-流纹岩的成因研究是认识地壳演化机制的重要途径.通过岩石学、地球化学和同位素地质学方法,对拉萨地体中部措麦地区灯垌破火山机构的火山-侵入杂岩进行了成因研究.灯垌火山-侵入杂岩主要由花岗斑岩、流纹岩和流纹质熔结凝灰岩组成,锆石SHRIMP U-Pb年龄分别为64.1±0.8 Ma、62.9±0.7 Ma和63.2±0.7 Ma,形成时代一致.他们同属高钾钙碱性准铝质-过铝质岩浆岩,亏损高场强元素、富集大离子亲石元素,轻稀土元素富集、重稀土元素平坦,具有一致的锆石δ18O值（6.15‰~7.34‰）,为同源岩浆演化的产物.流纹岩与花岗斑岩亏损Ba、Sr、P和Ti元素,具显著的负Eu异常,是岩浆发生不同程度分异演化的产物,前者代表晶粥体分离的熔体相,而后者是晶粥体富矿物相部分的产物.流纹质熔结凝灰岩轻重稀土元素分异程度相对较弱,具中等-弱的Eu负异常,是晶粥体自身被活化喷发的产物.结合前人研究成果,认为灯垌火山-侵入杂岩可能形成于古新世新特提斯洋北向俯冲于拉萨地体之下的过程中,俯冲带流体进入地幔楔并使其部分熔融,形成的幔源物质上涌,使地壳部分熔融形成的中酸性岩浆侵入或喷发而形成侵入岩或火山岩.   相似文献   

热带大气季节内振荡激发El Nino的机制   总被引：15，自引：1，他引：15  

李崇银  廖清海 《热带气象学报》1998,14(2):97-105

资料分析了表明,热带大气季节内振荡同Ｅｌ Ｎｉｎｏ发生有密切的关系。在Ｅｌ Ｎｉｎｏ事件发生之前,热带大气（尤其是赤道西太平洋地区）季节内振荡异常加强;伴随着Ｅｌ Ｎｉｎｏ的发生,热带大气季节内振荡动能明显增加。简单海－气耦合模式的分析表明,只有在年陵时间尺度大气外强迫作用下,海－气系统才可以产生类似ＥＮＳＯ模的耦合波。资料和理论模式分析和结果相结合,说明热带大气季节内振荡激发Ｅｌ Ｎｉｎｏ的机制  相似文献   

商用扫描仪在天文底片数字化中的测试     

于涌  赵建海  唐正宏  廖石龙 《天文研究与技术》2013,(3):288-292

我国的天文底片数字化工作已正式启动,选取高精度的扫描仪是该工作首要和基本的任务。对Epson公司的V750 Pro和10000XL,以及Phase One公司的PowerPhase FX+扫描仪开展了测试,结果表明,PowerPhase FX+具有较高的扫描精度,一方面,该扫描仪扫描方向的稳定性与线阵CCD方向相当,均优于0.5μm;另一方面,通过UCAC3参考星归算结果显示,尽管PowerPhase FX+的照相式扫描会带来像场畸变,但考虑3阶底片模型后,扫描星像的位置精度较高。对于上海天文台佘山40 cm折射望远镜1987年拍摄的M79底片,扫描星像的位置精度优于0.1″。  相似文献   

Geochronology of the Limu W–Sn–Nb–Ta‐Bearing Granite Pluton in South China     

Zuohai Feng  Zhiqiang Kang  Feng Yang  Jiafei Liao  Chunzeng Wang 《Resource Geology》2013,63(3):320-329

Limu W–Sn–Nb–Ta mining district is located in the Nanling Range W–Sn poly‐metallic mineralization belt in south China. The district includes a number of Sn–Nb–Ta and W–Sn ore occurrences; all of them are spatially associated with granite stocks of a largely‐unexposed pluton, the Limu granitic pluton. A granite sample collected from the Sn–Nb–Ta‐bearing Jinzhuyuan granite stock yields a zircon SHRIMP U–Pb age of 218.3 ± 2.4 Ma, a muscovite ⁴⁰Ar/³⁹Ar plateau age of 212.4 ± 1.4 Ma, and a muscovite ⁴⁰Ar/³⁹Ar isochron age of 213.2 ± 2.2 Ma. Another granite sample collected from the W–Sn‐bearing Sangehuangniu granite stock yields a zircon SHRIMP U–Pb age of 214 ± 5 Ma. The geochronological data provide new constraints on the age of the Limu granite pluton and the timing of the associated W–Sn–Nb–Ta mineralization—at least it sets a reasonable upper age limit for the mineralization of the W–Sn–Nb–Ta ores. The reported ages suggest an active Late Triassic granitic magmatism in Limu area which is part of a regional magmatic event near the end of the Indosinian orogeny in south China.  相似文献