各种大气水汽输送气候计算方法的比较和讨论   总被引：4，自引：0，他引：4  

史慧敏  林守廉 《南京气象学院学报》1994,17(3):372-378

比较瞬时法，平均法和逐层平均法３种水汽输送气候计算方案，发现它们的输送方向大致相同，输送量差异显著。瞬时法最准确；逐层平均法次之，但误差的年际波动较大，平均法虽然简单然而误差大。  相似文献   

Geochemistry　of　Thermal－Mineral　Waters　in　Siping＇an　District，　Shanxi　Province，　China     

Wan Yanxin  Sun Lianfa 《中国地质大学学报(英文版)》1994,(1)

ＧｅｏｃｈｅｍｉｓｔｒｙｏｆＴｈｅｒｍａｌ－ＭｉｎｅｒａｌＷａｔｅｒｓｉｎＳｉｐｉｎｇ＇ａｎＤｉｓｔｒｉｃｔ，ＳｈａｎｘｉＰｒｏｖｉｎｃｅ，Ｃｈｉｎａ￥ＷａｎＹａｎｘｉｎ；ＳｕｎＬｉａｎｆａ（ＤｅｐａｒｔｍｅｎｔｏｆＨｙｄｒｏｇｅｏｌｏｇｙａｎｄＥｎ...  相似文献   

Circulation and water masses of the Arabian Sea     

S. R. Shetye  A. D. Gouveia  S. S. C. Shenoi 《Journal of Earth System Science》1994,103(2):107-123

The dynamics and thermodynamics of the surface layer of the Arabian Sea, north of about 10N, are dominated by the monsoon-related annual cycle of air-sea fluxes of momentum and heat. The currents in open-sea regime of this layer can be largely accounted for by Ekman drift and the thermal field is dominated by local heat fluxes. The geostrophic currents in open-sea subsurface regime also show a seasonal cycle and there is some evidence that signatures of this cycle appear as deep as 1000 m. The forcing due to Ekman suction is an important mechanism for the geostrophic currents in the central and western parts of the Sea. Recent studies suggest that the eastern part is strongly influenced by the Rossby waves radiated by the Kelvin waves propagating along the west coast of India. The circulation in the coastal region off Oman is driven mainly by local winds and there is no remotely driven western boundary current. Local wind-driving is also important to the coastal circulation off western India during the southwest monsoon but not during the northeast monsoon when a strong (approximately 7 × 10⁶m³/sec) current moves poleward against weak winds. This current is driven by a pressure gradient which forms along this coast during the northeast monsoon due to either thermohaline-forcing or due to the arrival of Kelvin waves from the Bay of Bengal. The present speculation about flow of bottom water (deeper than about 3500 m) in the Arabian Sea is that it moves northward and upwells into the layer of North Indian Deep Water (approximately 1500–3500m). It is further speculated that the flow in this layer consists of a poleward western boundary current and a weak equatorward flow in the interior. It is not known if there is an annual cycle associated with the deep and the bottom water circulation.  相似文献   

The management of sewage sludge by the water industry in England and Wales     

R. A. Crichton 《Geotechnical and Geological Engineering》1994,12(3):183-212

Summary The legislative framework within which the disposal of sewage sludge is managed in England and Wales and the methods employed are outlined. Those factors which affect management decisions are analysed and consideration is given to the environmental implications of those decisions. Sewage processes and sludge disposal are considered, and the problems, especially those of heavy metal contamination, are addressed. An indication is given as to how the Water Services Companies are likely to implement the more stringent controls on disposal. Finally, the future of sludge management in England and Wales is discussed.Abbreviations BAT Best available technology - BATNEEC Best available technology not entailing excessive cost - BOD₅ Biochemical oxygen demand - BPEO Best practicable environmental option - CBI Confederation of British Industry - CEST Centre for Exploitation of Science and Technology - COD Chemical oxygen demand - CSC Customer Services Committee - DAF Dissolved air flotation - DG Director General - DoE Department of the Environment - DS Dried solids  相似文献   

Storm surge mitigation through vegetation canopies     

M. B. Danard  T. S. Murty 《Natural Hazards》1994,9(1-2):155-166

The paper of Reid and Whitaker (1976) on the effects of a vegetation canopy on flow of water is re-examined. Their assumptions on the equality of various drag coefficients are replaced by more realistic calculations. A new method for calculating wind stress on water is presented for the case when the vegetation extends above the water surface.For the case of vanishingly small water depth, it is shown that the horizontal stress is approximately constant in the vertical. This results in a diagnostic relationship for the water current as a function of the wind stress and bottom roughness.A new expression for the vertically averaged frictional force per unit mass is derived on the assumption that the friction velocity varies linearly with height. The vertical rate of change of friction velocity depends on the mean water current, the wind stress, the bottom roughness, and the water depth. This work has a possible application in the mitigation of storm surges.  相似文献   

塔克拉玛干沙漠中的古河道与地下水     

张鸿义  许风林 《新疆地质》1994,(3)

塔克拉玛干沙漠中发育有众多的古河道，其密集区主要集中在大沙漠中部。不同河流的古河道，含水层岩性有明显差异，地下水的富水性也明显不同。但沿古河道，地下水富水性均较两侧好，水质也相对较好，多为淡水和微咸水，为在沙漠区寻找水资源提供了方向  相似文献   

对饱和粘性土渗透规律的新认识及其应用     

Su Qingshan  Hou Jie  Duan tment of Hydrogeology  Engineering Geology) 《吉林大学学报(地球科学版)》1994,(1)

通过实验，对饱和粘性土的渗透规律进行研究，得到几点新认识。利用此认识建立了饱和粘性土越流补给量的计算公式，并在实际应用中得到验证。  相似文献   

电法勘探在常德市松散孔隙含水层中涌水量预测的应用     

李一之 《湖南地质》1994,13(3):171-173

常德市水文地质及电测深、电测井的资料反映了孔隙水含水层涌水量的大小与含水层厚度、颗粒组分及其结构的多因素的复杂组合──—厚度（Ｍ）与视电阻率（ρ＿ｓ）的乘积密切相关，据此可预测单井涌水量。  相似文献   

干法毛管压力试验新技术及其在判别储层水饱和度中的应用   总被引：1，自引：0，他引：1  

向阳  单钰铭  赵冠军 《矿物岩石》1994,(2)

根据毛细管压力理论研制的ＹＢ－１型岩石水饱和度仪，广泛应用于油气勘探开发中测定储集岩石的含水饱和度，测定误差小于５％，该方法为不受取心条件、样品大小、物性和岩性限制快速的新方法，实际应用证明效果较好  相似文献   

上海夏灌水现状及其开发利用     

万贵富  龚士良  叶玲玲  寿鸿祥 《上海国土资源》1994,(4)

本文对上海市区地下含水层中滞留的夏灌余水的现状进行了调查分析与评价,对其开发利用的可行性作了论证,以助于今后更好地开展“夏灌冬用”工作。  相似文献