地热储层单裂隙岩体渗流传热数值模拟研究          下载免费PDF全文

肖鹏  窦斌  田红  郑君  崔国栋  夏杰勤  Muhammad Kashif 《探矿工程》2021,48(2):16-28

研究地热储层裂隙岩体中的渗流传热过程对干热岩地热资源的开采具有重要的意义。本文以干热岩地热工程为背景,采用COMSOL Multiphysics数值模拟软件对地热储层单裂隙岩体中渗流传热机理进行了研究,并分析了流体注入速度和温度对岩体温度场的影响及其对干热岩地热工程的影响。研究发现流体参数对岩体温度场的影响主要体现在两个方面：一方面是对岩体温度场受扰动区域以及幅度的影响,另一方面是对岩体温度场达到稳态所需要时间的影响。流体注入速度的提升会降低系统的寿命和寿命期的出口法向总热量值,当考虑出口法向总热通量时,存在最佳流体注入速度,本研究中最佳流体注入速度为0.011m/s。流体注入温度的提升会增加系统的寿命和系统的出口法向总热通量和总热量。研究为干热岩自热资源的开发与利用提供了理论依据,为工程运行参数的设计提供了参考依据。  相似文献   

贵州岩溶疏干区浅层地热能地埋管施工技术          下载免费PDF全文

陈浩  赵华宣  贾玉川  曾远明  汤自华  王虎  李勇 《探矿工程》2021,48(3):170-177

贵州省浅层地热能资源丰富,开发潜力巨大,但碳酸盐岩地层分布广、浅表岩溶裂隙极为发育,浅层地埋管施工难度大。以贵州仁怀妇幼保健院浅层地温中央空调地埋管工程为例,采用偏心潜孔锤跟管钻进、潜孔锤钻进、简便除尘器除尘、固结封堵和圆木封隔溶洞、提吊法下管等技术措施,解决了在由于溶蚀和断裂构造及河流深切割作用造成的局部岩溶发育以及地埋管埋置深度内无水的岩溶疏干区进行地埋管施工面临的松散浅表回填及岩溶软弱层成孔困难、全孔段无液面潜孔锤钻进粉尘污染环境、溶洞跑管（PE管）等技术难题,在保证了工程质量、安全的同时提高了施工效率,为类似工程提供了施工经验。  相似文献   

组分对铁基金刚石钻头的力学性能影响研究          下载免费PDF全文

刘冀 《探矿工程》2021,48(5):47-53

为提高金刚石钻头钻进钢筋混凝土、强磨性岩层的钻进效率,选择了一种耐磨性高、冷压成型好的铁预合金粉。本文设计了铁基胎体配方,研究了铁基预合金粉、Cu、Ni、Co各成分对铁基金刚石钻头胎体及钻进性能的影响。测试了不同配方下烧结试样的抗拉强度、三点抗弯强度和硬度,使用扫描电镜对断口进行微观分析,通过现场钻进实验测试钻头的钻进效率与寿命。同时分析了保温时间对铁基胎体力学性能的影响。结果表明：Cu、Ni、Co对铁基胎体的抗弯强度和硬度影响较大,且保温时间为5 min时,铁基胎体可以获得较好的力学性能。  相似文献   

北太平洋副热带东部模态水现在和未来的模拟分析   总被引：2，自引：1，他引：1  

XIA Ruibin  LIU Qinyu  XU Lixiao  LU Yiqun 《海洋学报(英文版)》2015,34(3):25-30

The present climate simulation and future projection of the Eastern Subtropical Mode Water(ESTMW) in the North Pacific are investigated based on the Geophysical Fluid Dynamics Laboratory Earth System Model(GFDL-ESM2M). Spatial patterns of the mixed layer depth(MLD) in the eastern subtropical North Pacific and the ESTMW are well simulated using this model. Compared with historical simulation, the ESTMW is produced at lighter isopycnal surfaces and its total volume is decreased in the RCP8.5 runs, because the subduction rate of the ESTMW decreases by 0.82×10-6 m/s during February–March. In addition, it is found that the lateral induction decreasing is approximately four times more than the Ekman pumping, and thus it plays a dominant role in the decreased subduction rate associated with global warming. Moreover, the MLD during February–March is banded shoaling in response to global warming, extending northeastward from the east of the Hawaii Islands(20°N, 155°W) to the west coast of North America(30°N, 125°W), with a maximum shoaling of 50 m, and then leads to the lateral induction reduction. Meanwhile, the increased northeastward surface warm current to the east of Hawaii helps strengthen of the local upper ocean stratification and induces the banded shoaling MLD under warmer climate. This new finding indicates that the ocean surface currents play an important role in the response of the MLD and the ESTMW to global warming.  相似文献   

世界大洋中绝热运动导致的纬向翻转环流和纬向热输送     

谭伟  黄瑞新  王卫强  王鑫 《海洋学报(英文版)》2015,34(11):80-91

Zonal overturning circulation(ZOC) and its associated zonal heat flux(ZHF) are important components of the oceanic circulation and climate system, although these conceptions have not received adequate attentions.Heaving induced by inter-annual and decadal wind stress perturbations can give rise to anomalous ZOC and ZHF.Based on a simple reduced gravity model, the anomalous ZOC and ZHF induced by idealized heaving modes in the world oceans are studied. For example, in a Pacific-like model basin intensified equatorial easterly on decadal time scales can lead to a negative ZOC with a non-negligible magnitude(–0.3×106 m3/s) and a considerable westward ZHF with an amplitude of –11.2 TW. Thus, anomalous ZOC and ZHF may consist of a major part of climate signals on decadal time scales and thus play an important role in the oceanic circulation and climate change.  相似文献   

2010年马卡罗夫海盆冰站观测期间垂向热通量时间变化研究   总被引：1，自引：1，他引：0  

郭桂军  史久新  矫玉田 《海洋学报(英文版)》2015,34(11):118-125

Based on hydrographic data obtained at an ice camp deployed in the Makarov Basin by the 4th Chinese Arctic Research Expedition in August of 2010, temporal variability of vertical heat flux in the upper ocean of the Makarov Basin is investigated together with its impacts on sea ice melt and evolution of heat content in the remnant of winter mixed layer(r WML). The upper ocean of the Makarov Basin under sea ice is vertically stratified. Oceanic heat flux from mixed layer(ML) to ice evolves in three stages as a response to air temperature changes, fluctuating from 12.4 W/m2 to the maximum 43.6 W/m2. The heat transferred upward from ML can support(0.7±0.3) cm/d ice melt rate on average, and daily variability of melt rate agrees well with the observed results. Downward heat flux from ML across the base of ML is much less, only 0.87 W/m2, due to enhanced stratification in the seasonal halocline under ML caused by sea ice melt, indicating that increasing solar heat entering summer ML is mainly used to melt sea ice, with a small proportion transferred downward and stored in the r WML. Heat flux from ML into r WML changes in two phases caused by abrupt air cooling with a day lag. Meanwhile, upward heat flux from Atlantic water(AW) across the base of r WML, even though obstructed by the cold halocline layer(CHL), reaches0.18 W/m2 on average with no obvious changing pattern and is also trapped by the r WML. Upward heat flux from deep AW is higher than generally supposed value near 0, as the existence of r WML enlarges the temperature gradient between surface water and CHL. Acting as a reservoir of heat transferred from both ML and AW, the increasing heat content of r WML can delay the onset of sea ice freezing.  相似文献   

成都、重庆城市热岛效应特征对比   总被引：1，自引：0，他引：1  

李晓敏  曾胜兰 《气象科技》2015,43(5):888-897

随着我国内陆地区城市化进程的加快,部分城市热岛效应的强度及范围都显著增强。应用MODIS地表温度数据从时空两个角度对成都、重庆两市的城市热岛效应现状及其演变进行对比分析。研究结果表明：①成都和重庆市的城市热岛效应明显,成都和重庆市热岛强度分别可达到4.32 ℃和3.11 ℃。空间上,成都市的城市热岛效应呈现环状分布特征;而重庆市呈现西北高东南低的分布特征;②4个季节中,春季成都、重庆的热岛强度分别为4.32 ℃和3.11 ℃,远高于其他3季的热岛强度;而春、秋、冬季成都的热岛强度都强于重庆;③年际变化来看,成都、重庆两地城市热岛效应范围在10年间呈现扩大趋势。其中成都弱热岛和中等热岛的范围有所减小,强热岛和极强热岛分布范围则有明显扩大;相反,重庆弱热岛和中等热岛的范围扩大,强热岛和极强热岛分布范围则明显减小。  相似文献   

Different Warming Patterns of Tropical Pacific Sea Surface Temperature Projected by FGOALS-g2 and FGOALS-s2 under RCP8.5          下载免费PDF全文

ZHANG Li-Xia  ZHOU Tian-Jun 《大气和海洋科学快报》2015,8(2):82-87

The different patterns of SST changes under the +8.5 W m-2 Representative Concentration Pathway(RCP8.5) projected by the latest two versions of the Flexible Global Ocean-Atmosphere-Land System model(FGOALS-g2 and FGOALS-s2; grid-point version 2 and spectral version 2, respectively), and the potential mechanisms for their formation are studied in this paper. The results show that, although both FGOALS-g2 and FGOALS-s2 project global warming patterns, FGOALS-g2(FGOALS-s2) projects a La Nia-like(an El Nio-like) mean warming pattern with weakest(strongest) warming over the central(eastern) equatorial Pacific for 2081–2100 relative to 1986–2005 under RCP8.5. A mixed layer heat budget analysis shows that the projected tropical Pacific Ocean warming in both models is primarily caused by atmospheric forcing. The main differences in the heating terms contributing to the SST changes between the two models are seen in the downward longwave radiation and ocean forcing. The minimum SST warming over the equatorial Pacific in FGOALS-g2 is attributed to the local minimum heating of downward longwave radiation and maximum cooling of ocean forcing. In contrast, the maximum SST warming over the equatorial Pacific in FGOALS-s2 is due to the maximum warming of downward longwave radiation, and the contribution of ocean forcing is minor. The minimum SST warming over the equatorial Pacific in FGOALS-g2 emerges around the 2050 s, before when the SST over the equatorial Pacific is warmer than that over the extra-equatorial Pacific. In FGOALS-s2, the SST difference shows a continuous increasing trend for 2006– 2100. Further examination of the oceanic and atmospheric circulation changes is needed to reveal the process responsible for the longwave radiation and ocean forcing difference between the two models.  相似文献   

Mass Human Migration and the Urban Heat Island during the Chinese New Year Holiday: A Case Study in Harbin City,Northeast China          下载免费PDF全文

WU Ling-Yun  ZHANG Jing-Yong  SHI Chun-Xiang 《大气和海洋科学快报》2015,8(2)

Many Chinese people leave big cities for family reunions during the Chinese New Year(CNY), which is the most important public holiday in China. However, how modern mass human migration during the CNY holiday affects the urban heat island(UHI) is still unknown. Here, the authors investigate the role of modern human migration for the UHI effects during the CNY holiday for the period of 1992–2006 in Harbin City, Northeast China. The results show that during the CNY week, the UHI effects expressed as daily mean, maximum, and minimum temperature differences between urban and rural stations averaged over the period of 1992–2006 are 0.65°C(43%), 0.31°C(48%), and 1.14°C(71%) lower than during the background period(four weeks before and four weeks after the CNY week), respectively. Our findings identify previously unknown impacts of modern mass human migration on the UHI effects based on a case study in Harbin City.  相似文献   

Quadrant-Averaged Structure and Evolution Mechanisms of a Northeast Cold Vortex during Its Mature Stage          下载免费PDF全文

LI Wei  SHEN Xin-Yong  FU Shen-Ming  LI Wan-Li 《大气和海洋科学快报》2015,8(1):45-51

A Northeast China cold vortex(NCCV) that maintained from 0200 UTC 3 July to 0500 UTC 3 July 2013 and caused several heavy rainfall events was analyzed in detail to reveal its quadrant-averaged structure and main maintaining mechanisms during its mature stage. Results indicated the vortex’s intensity, divergence, ascending motions, precipitable water(PW), and thermal structures were all characterized by significant unevenness, and their main pattern changed gradually during the mature stage. Mechanisms accounting for the maintenance of the NCCV were also characterized by remarkable unevenness. Within different quadrants, dominant factors for the vortex’s evolution may have differed from each other significantly. The NCCV-averaged vorticity budget revealed that the vertical advection of vorticity, which is closely related to convective activities, was the most favorable factor for maintaining the NCCV, whereas the tilting effect, which is closely related to the vertical shear of the horizontal wind(horizontal vorticity), was the most detrimental factor.  相似文献