Coupling of a biogeochemical model with a simultaneous heat and water model and its evaluation at an alpine meadow site   总被引：2，自引：0，他引：2  

Xufeng Wang  Mingguo Ma  Yi Song  Junlei Tan  Haibo Wang 《Environmental Earth Sciences》2014,72(10):4085-4096

Alpine meadow covers most of the Qinghai-Tibet Plateau where frozen soil is widely distributed. In order to correctly simulate the carbon, water and energy flux of an alpine meadow site at Qinghai-Tibet Plateau, a widely used carbon cycle model Biome-BGC and a cold region land surface model SHAW were coupled. The outputs of the coupled model were validated with the observed carbon fluxes (Gross Primary Productivity, Net Ecosystem Exchange, Ecosystem Respiration), energy fluxes (Latent heat flux, Sensible heat flux), water flux (Evapotranspiration), soil moisture and soil temperature at A’rou site which is located on the east edge of Qinghai-Tibet Plateau. The results indicate that the coupled model can correctly predict the interactions between alpine meadow ecosystem and atmosphere.  相似文献   

福建永泰无岩坑钼矿地质特征及成因探讨     

谭元松 《福建地质》2010,29(2):101-106

永泰无岩坑钼矿体贮存于成矿母岩燕山晚期中粗粒含黑云母花岗岩边缘相细晶质花岗岩硅化褪色蚀变带中,储矿构造主要为花岗岩岩体顶部的内接触带即岩凸构造,以及区域性北西向断裂的次级裂隙。矿床成因属岩浆期后热液充填型。  相似文献   

云南仙人洞文石类石笋年层结构电镜分析     

段武辉  谭明  程海  张勇 《第四纪研究》2010,30(5)

关于文石类石笋年层的研究,国外曾有报道.Brook等[1]发现马达加斯加岛的一根石笋,其微层由亮色(clear)的文石亚层和暗色(darker)的文石亚层互层组成,而后Bertaux等[2]又在巴西发现了类似的石笋微层,经过分析,均认为每对明暗相间的亚层组成一个年层,并指出暗色亚层可能是由于文石晶体中混入了粘土或者有机质造成的.  相似文献   

甘肃武都万象洞石笋双重光性微层特征     

袁野  白益军  桑文翠  段武辉  张德忠  谭明  张平中  程海 《第四纪研究》2010,30(6)

自1993年Baker等利用高精度TIM S-U系法对Tartair洞一根全新世石笋的发光条带进行年代测定,并通过计数证明其为年生长层之后,石笋微层以其明确的年代学意义和气候环境变化指示意义,逐渐被成功地应用于古气候的定量重建;1995年在北京石花洞国内首次发现石笋微层后,我国学者也开始逐渐关注石笋微层气候学,并对其进行了全面和系统的研究.我国已观测到的石笋微生长层大致可分为"北方型"和"南方型"两种,其中"北方型',微层主要分布在东部地区,在北京石花洞、银狐洞、本溪水洞、南京葫芦洞、山东开元洞等地均已发现,但在我国西部地区尚未见石笋微生长层的报道.最近,笔者在2007年3月采自中国西部青藏高原和黄土高原过渡带万象洞(33019'N,105000'E;海拔1200m)中的一根石笋中发现了典型的"北方型"微生长层.  相似文献   

不同变质变形煤储层孔隙特征与煤层气可采性   总被引：3，自引：0，他引：3  

范俊佳  琚宜文  侯泉林  谭静强  卫明明 《地学前缘》2010,17(5):325

煤储层孔隙是煤层气的主要聚集场所和运移通道,煤储层孔隙结构不仅制约着煤层气的含气量,而且对其可采性也有重要影响。文中选取淮北煤田和沁水盆地不同矿区有代表性的煤样,通过对研究区不同变质与变形煤样的宏微观构造观测、镜质组反射率与孔隙度测试以及压汞实验分析,研究了不同变质变形煤储层孔隙结构特征及其对煤层气可采性的制约。研究结果表明,按照不同的变质变形特征将研究区煤储层主要划分为5类,即:高变质较强至强变形程度煤储层(Ⅰ类)、高变质较弱变形程度煤储层(Ⅱ类)、中变质较强变形程度煤储层(Ⅲ类)、中变质较弱变形程度煤储层(Ⅳ类)及低变质强变形程度煤储层(Ⅴ类)。不同变质变形煤储层的孔隙结构具有以下特征:Ⅰ类和Ⅱ类煤储层吸附孔占主导,Ⅰ类煤储层孔隙连通性差,Ⅱ类煤储层因后期叠加了构造裂隙,孔隙连通性变好;Ⅲ类煤储层中孔、大孔增多,但有效孔隙少,孔隙连通性变差;Ⅳ类煤储层吸附孔较多,中孔、大孔中等,且煤储层内生裂隙发育,孔隙具有较好的连通性,渗透性明显变好;Ⅴ类煤储层吸附孔含量较低,中孔较发育,大孔不太发育,有效孔隙少,孔隙连通性差。由此,变质程度高且叠加了一定构造变形的煤储层(Ⅱ类)以及中等变质程度变形较弱且内生裂隙发育的煤储层(Ⅳ类),其煤层气有较好的渗透性,可采性较好。  相似文献   

高矮建筑物多上行先导连接过程的数值模拟          下载免费PDF全文

雷艺楠  谭涌波  余骏皓  郑天雪 《应用气象学报》2022,33(1):80-91

运用改进后的三维多先导模型,允许高矮建筑物上均可以始发上行先导,对多次地闪的连接过程进行模拟.结果 表明:矮建筑物始发上行先导和被击中的概率较小,高建筑物对矮建筑物上行先导的始发具有较明确影响.建筑物间的高度差是影响上述连接过程的主要因子,当建筑物间高度差较小时,高建筑物对矮建筑物的屏蔽效应不明显,下行先导通道的相对位...  相似文献   

An ERDAS image processing method for retrieving LST and describing urban heat evolution: a case study in the Pearl River Delta Region in South China     

Qinqin Sun  Jianjun Tan  Yonghang Xu 《Environmental Earth Sciences》2010,59(5):1047-1055

A spatial-temporal model with Model Maker tool is designed to retrieve Land Surface Temperature (LST) and to describe the changes of urban heat island, as well as urban development. Spectral Radiance, Brightness Temperature, NDVI, and Emissivity are first calculated from TM and ETM+, which are then used to compute LST by using Qin et al.’s mono-window algorithm. The LST is classified based on normalized statistical method, and the normalized heat images are computed between different times. Therefore, the urban heat changes can be shown in the map clearly and directly through an urban heat conversion matrix. Such a model has been applied in this study to obtain the urban heat conversion matrix of South China from 1990 to 2000. The results indicate that the LST increased areas mainly locate along the major roads in the eastern bank of the Pearl River, which is a result of speedy urban expansion and need to be noticed in the future.  相似文献   

Palaeomagnetism of Early Triassic limestones from the Huanan Block, South China: no evidence for separation between the Huanan and Yangtze blocks during the Early Mesozoic   总被引：1，自引：0，他引：1  

Xiaodong Tan  Kenneth P. Kodama  Pengyan Wang  & Dajun Fang 《Geophysical Journal International》2000,142(1):241-256

  相似文献   

东昆仑东段加里东造山旋回侵入岩特征研究     

拜永山  常革红  谈生祥  王进寿 《青海国土经略》2001,(Z1)

新一轮区调填图所获资料表明,加里东期花岗岩成因类型复杂多样,有岛弧花岗岩、同碰撞花岗岩及少量陆内造山花岗岩等,说明东昆仑东段在加里东时期经历了复杂的洋—陆俯冲、陆陆碰撞的动力学过程。  相似文献   

Summer heat waves over western Turkey between 1965 and 2006     

Yurdanur Sezginer Unal  Elcin Tan  S. Sibel Mentes 《Theoretical and Applied Climatology》2013,112(1-2):339-350

Global warming is one of the greatest environmental, economic, and social threats in the world. There are many assessments to estimate climate variability over many regions. A change in the Earth’s surface temperature leads to increase in extreme temperature events, which are harmful to the ecosystem, and moreover, they create danger on human health. In this study, we have selected the western part of Turkey as the study area, since climate change projections for Turkey point out that the highest temperature change can be expected on this region during summer, and the Turkish population is very dense here to be affected by extreme events. We have used apparent temperatures to define the heat waves which we have determined their frequencies for the summer months (June–August) of 1965–2006. Since the regional comparisons of station results are intended, we selected the 90th percentile value for each station as a threshold value to be used in the delineation of heat waves. Then, the number of heat waves is determined by imposing the constraint that apparent temperatures stay above the threshold value at least for three consecutive days. Then, the changes in the number of hot days and heat waves and also their durations are analyzed by using the linear least square method. We have found that the number of hot days, heat waves, and heat wave durations is increased between 1965 and 2006 on the western part of Turkey. Additionally, their rate of change is larger within the last decade and extremes are frequently observed after 1998. Regional distributions show that the tendency of the number of heat wave events increases towards the southern latitudes of the domain. Moreover, we investigated the relationship between the number of hot days and the sea surface temperatures of the Mediterranean Sea and Black Sea. Correlation analyses are carried out by the number of hot days and averaged sea surface temperatures on the regions of the western, central, and eastern Mediterranean Sea and the Black Sea. It is found that the number of hot days of west Turkey is better correlated with the sea surface temperatures averaged over eastern Mediterranean and Black Seas. The number of heat waves is found significantly correlated with the fire occurrences for most of the stations.  相似文献