潜水搅拌机分布对污水处理池搅拌效果的影响

为研究潜水搅拌机的分布对污水处理池内搅拌效果的影响,采用三维建模软件Pro/E建立实体模型,利用ICEM大型软件对污水处理池进行非结构化四面体网格划分,在Fluent 6.3计算流体力学软件平台上,采用动坐标系技术、RNG k-ε湍流模型和PIOS算法,对潜水搅拌机搅拌的污水处理池进行数值模拟,分析全池内流体的宏观流场与各截面速度流场分布,考察各潜水搅拌机的效率,同时对污水处理池内的流体平均速度及搅拌面积率进行了研究.计算结果表明:优选方案H中,3个潜水搅拌机转速为1 200 r/min,安装角度分别为45°,30°,30°,其搅拌面积率超过90%.在3个潜水搅拌机搅拌下,污水处理池内流体形成连续循环水流,搅拌充分,平均流速在0.3 m/s左右,符合潜水搅拌机工作要求.利用此方法,可为潜水搅拌机的实际工程应用提供参考依据.

老贵阳的餐馆

题中老贵阳,指的是上世纪50至70年代的贵阳。我生于此长于此,对当时的贵阳还有印象。在那个物质生活条件相当匮乏的年代,人们对“吃”特别在乎,作为少年儿童的我,自然对“吃”的印象较其他方面深刻。50年代,学龄前的我没有条件去认识餐馆,只依稀记得曾在家长带领下,到一个大饭店参加某位长辈的婚宴,这可是我人生第一次进餐厅,贵阳话叫“开洋荤”。我记得饭店内有个大水池,养着不少大鱼,这是我第一次看见几斤重的活鱼。稍懂事后问父亲,才知道这是贵阳有名的贵阳饭店(位于喷水池)。至今还在,只是面目全非了。

这儿真美

北海公园是个好地方,这儿真美.一进北海公园,我就看到了一座漂亮的假山.假山又叫佛光山,山上的石头奇形怪状,山顶上生长着几棵松树.山里面是曲曲折折的山洞,小孩可以在里面玩耍,大人可以在里面乘凉.假山前面有一个大水池,水池里有三块奇石:左边是龟石,右边是蛙石,中间那块是鳄鱼石.

某综合体的消防水系统设计简析

本文以实际超高层工程为例,从消防用水量、消防水池及泵房、系统管网设计等方面介绍了该项目的消防水系统设计,并重点介绍该项目的特点:高位消防大水池、常高压水消防系统等技术,同时强调了超高层建筑的消防设施的重要性及安全可靠性。

Optimization of Bow Shape for a Non Ballast Water Ship

In this research,a commercial CFD code ＂Fluent＂ was applied to optimization of bulbous bow shape for a non ballast water ships（NBS）.The ship was developed at the Laboratory of the authors in Osaka Prefecture University,Japan.At first,accuracy of the CFD code was validated by comparing the CFD results with experimental results at towing tank of Osaka Prefecture University.In the optimizing process,the resistances acting on ships in calm water and in regular head waves were defined as the object function.Following features of bulbous bow shapes were considered as design parameters： volume of bulbous bow,height of its volume center,angle of bow bottom,and length of bulbous bow.When referring to the computed results given by the CFD like resistance,pressure and wave pattern made by ships in calm water and in waves,an optimal bow shape for ships was discovered by comparing the results in the series of bow shapes.In the computation on waves,the ship is in fully captured condition because shorter waves,λ/Lpp 0.6,are assumed.

Interdecadal Variability in Large and Small Warm Pools in Western Pacific and Their Association with Rainfall Anomalies

This study investigated interdecadal variability of June–October(JJASO) the large and small warm pools in western Pacific and their association with rainfall anomalies using station and reanalysis data from 1958 to 2008.The results indicated that the large and small warm pools in western Pacific showed an interdecadal shift around 1986.The large warm pool years over western Pacific were found after 1986,whereas the small warm pool years were often seen throughout the periods before 1986.The analysis results also showed that there were obvious interdecadal variability in JJASO rainfall in Southeast China and warm pool in western Pacific.During 1958–1985(small warm pool years),the decrease in rainfall was associated with tropospheric moisture divergence and sinking motion over Southeast China and warm pool in western Pacific.However,during 1986–2008(large warm pool years),the increase in rainfall was associated with tropospheric moisture convergence and ascending motion.Further analysis showed that large warm pool contributed to the increase in surface latent heat fluxes over warm pool in the western Pacific.Thus,there was an increase in the amount of water vapor over Southeast China and warm pool in western Pacific,which contributed to increased rainfall in these regions.

Assessment of Water Microbiologic Pollution in Durres＇s Marine Harbour Basin, Albania

The aim of this study is to assess the water microbiologic pollution in Durres＇s Harbour basin and to compare it with European standards. The comparison of heterotrophs and total coliforms level in sampling are the essence of this research. The object of this study is done in four sampling areas of Durres＇s Harbour basin. In order to compare the level of water microbiologic pollution in four areas of Durres＇s Harbour basin, control area is also studied which is a beach area near the Harbour named Apollonia Beach. The sampling areas were： Ferry Terminal （FT）, Fishery Harbor （FH）, East Zone （EZ）, Fuel Quay （FQ） and Apollonia Beach （AB）, respectively. The period of sample-taking was July-October 2008. The strategy used for this purpose consisted in water insemination with coverage method by means of Petri＇s plates according to respective dilutions in culture media Plate Count Agar （PCA） for heterotrophs and MacConkey for total coliforms. The number of colonies that are formed determines the number of cells at the moment of water insemination, the number of heterotrophs in culture media PCA, respectively. The number of pink and red colonies that were formed determines the number of cells at the moment of water insemination, the number of total coliforms in culture media MacConkey, respectively. The measure ofheterotrophic bacteria and total coliforms used is Colony-Forming Units （CFU）/100 mL seawater. （AB） is within European standards. The richest area with heterotrophs is （FH）, which confirms the fact that it is the most polluted microbiologic area in the Harbour basin of Durres. The richest area with total coliforms is （FT）. The poorest area with heterotrophs and total coliforms is （FQ）.

Removal of Iron, Coliforms and Acidity from Ground Water Obtained from Shallow Aquifer Using Trickling Filter Method

Ground water is a major source of drinking water. In the Niger Delta, the ground water is unfit for human consumption due to high concentration of iron, coliforms and acidity. In an attempt to make the water potable, groundwater samples were collected from domestic boreholes and analyzed for physicochemical and microbial parameters using standard analytical methods. The groundwater samples were collected after single and double trickling filter treatment. The treated water from the single and double trickling filter was similarly analyzed. Results show that after treatment, iron decreased from 5.23-9.96 mg/L in the raw water to 1.67-2.02 mg/L in the single treatment and 0.05-0.31 mg/L in the double treated water （P 〈 0.05）. Similarly, pH increased from 4.39-5.17 in the raw water to 5.31-5.87 in the single treatment and 6.09-6.90 in the double treatment （P 〈 0.05）. Coliforms decreased from 60-85 MPN/100 mL in the raw water to 3-10 MPN/100 mL in the single treatment and 0-2 MPN/100 mL in the double treatment （P 〈 0.05）. Based on the findings of this study, it is recommended that it is unsafe to drink untreated groundwater as currently practiced in the Niger Delta, but should be subjected to double trickling filter treatment and chlorination before consumption.

Photovoltaic Powered Reverse Osmosis Plant for Brackish Water without Batteries with Self Acting Pressure Valve and MPPT

This paper presents a PV （photovoltaic） powered RO （reverse osmosis） plant for brackish water without batteries and a self-regulating pressure valve. The aim is to extract the maximum power from the PV module using an MPPT （maximum power point tracking） technique for powering a solar water pump and maintain constant the pressure in the RO membranes by using the self-operated valve. A Buck type converter using the InCond （incremental conductance） MPPT was developed for this application. The MPPT chosen was simulated, tested and validated, showing an efficiency of 86.8%. The technical feasibility of the RO plant was made by PLC （programmable logic controller） and was tested for two salinity levels （1,000 and 1,500 mg/L of TDS （total dissolved solids））. These salinity levels chosen are commonly found in most brackish water wells of the semi-arid region of Northeastern Brazil. The RO plant could permeate 175.3 L/day of drinking water with 120 mg/L of TDS and specific energy consumption of 2.56 kWh/m3.

2003年5月号“趣题有奖竞答”答案

《巧拼图形》略.《乱中求实》设质量为1 g、10 g、50 g的木块数分别为x、Y、z,则x+y+z=100,x+10y+50z=500. ②-①,得9y+49z=400,故y=44-5z+4×(1-z)/9.因y、z均为正整数,故(1-z)/9为整数.设(1-z)/9=t(t为整数),则z=1-9t,y=39+49t.而-39/40<t<1/9,故t=0,z=1,

Climatic features of atmospheric heat source/sink over the Qinghai-Xizang Plateau in 35 years and its relation to rainfall in China

Using the 1961–1995 monthly averaged meteorological data from 148 surface stations in the Qinghai-Xizang Plateau (QXP) and its surrounding areas, calculation of the 35-year atmospheric heat source/sink (<Qi>) and an analysis on its climatic features and relation to rainfall in China have been made. It is found that on the average, the atmospheric heat source over the QXP is the strongest in June (78 W / m2) and cold source is the strongest in December (?72 W/m2). The sensible heat of the surface increases remarkably over the southwest of the QXP, causing the obvious increase of <Qi> there in February and March, which makes a center of the atmospheric heat source appear over the north slope of the Himalayas. Afterwards, this center continues to intensify and experiences noticeable migration westwards twice, separately occurring in April and June. The time when the atmosphere over the east of the QXP becomes heat source and reaches strongest is one month later than that over the southwest of the QXP. In summer, the latent heat of condensation becomes a heating factor as important as the sensible heat and is also a main factor that makes the atmospheric heat source over the east of the QXP continue growing. On the interdecadal time scale, (Q1) of the QXP shows an abrupt change in 1977 and a remarkable increase after 1977. The atmospheric heat source of the spring over the QXP is a good indicator for the subsequent summer rainfall over the valleys of the Changjiang and Huaihe rivers and South China and North China. There is remarkable positive correlation between the QXP heat source of summer and the summer rainfall in the valleys of the Changjiang River.

Carbon pools and fluxes in the China Seas and adjacent oceans

The China Seas include the South China Sea, East China Sea, Yellow Sea, and Bohai Sea. Located off the Northwestern Pacific margin, covering 4700000 km^2 from tropical to northern temperate zones, and including a variety of continental margins/basins and depths, the China Seas provide typical cases for carbon budget studies. The South China Sea being a deep basin and part of the Western Pacific Warm Pool is characterized by oceanic features; the East China Sea with a wide continental shelf, enormous terrestrial discharges and open margins to the West Pacific, is featured by strong cross-shelf materials transport; the Yellow Sea is featured by the confluence of cold and warm waters; and the Bohai Sea is a shallow semiclosed gulf with strong impacts of human activities. Three large rivers, the Yangtze River, Yellow River, and Pearl River, flow into the East China Sea, the Bohai Sea, and the South China Sea, respectively. The Kuroshio Current at the outer margin of the Chinese continental shelf is one of the two major western boundary currents of the world oceans and its strength and position directly affect the regional climate of China. These characteristics make the China Seas a typical case of marginal seas to study carbon storage and fluxes. This paper systematically analyzes the literature data on the carbon pools and fluxes of the Bohai Sea,Yellow Sea, East China Sea, and South China Sea, including different interfaces(land-sea, sea-air, sediment-water, and marginal sea-open ocean) and different ecosystems(mangroves, wetland, seagrass beds, macroalgae mariculture, coral reefs, euphotic zones, and water column). Among the four seas, the Bohai Sea and South China Sea are acting as CO_2 sources, releasing about0.22 and 13.86–33.60 Tg C yr^(-1) into the atmosphere, respectively, whereas the Yellow Sea and East China Sea are acting as carbon sinks, absorbing about 1.15 and 6.92–23.30 Tg C yr^(-1) of atmospheric CO_2, respectively. Overall, if only the CO_2 exchange at the sea-air interface is considered, the Chinese marginal seas appear to be a source of atmospheric CO_2, with a net release of 6.01–9.33 Tg C yr^(-1), mainly from the inputs of rivers and adjacent oceans. The riverine dissolved inorganic carbon (DIC) input into the Bohai Sea and Yellow Sea, East China Sea, and South China Sea are 5.04, 14.60, and 40.14 Tg C yr^(-1),respectively. The DIC input from adjacent oceans is as high as 144.81 Tg C yr^(-1), significantly exceeding the carbon released from the seas to the atmosphere. In terms of output, the depositional fluxes of organic carbon in the Bohai Sea, Yellow Sea, East China Sea, and South China Sea are 2.00, 3.60, 7.40, and 5.92 Tg C yr^(-1), respectively. The fluxes of organic carbon from the East China Sea and South China Sea to the adjacent oceans are 15.25–36.70 and 43.93 Tg C yr^(-1), respectively. The annual carbon storage of mangroves, wetlands, and seagrass in Chinese coastal waters is 0.36–1.75 Tg C yr^(-1), with a dissolved organic carbon(DOC) output from seagrass beds of up to 0.59 Tg C yr^(-1). Removable organic carbon flux by Chinese macroalgae mariculture account for 0.68 Tg C yr^(-1) and the associated POC depositional and DOC releasing fluxes are 0.14 and 0.82 Tg C yr^(-1), respectively. Thus, in total, the annual output of organic carbon, which is mainly DOC, in the China Seas is 81.72–104.56 Tg C yr^(-1). The DOC efflux from the East China Sea to the adjacent oceans is 15.00–35.00 Tg C yr^(-1). The DOC efflux from the South China Sea is 31.39 Tg C yr^(-1). Although the marginal China Seas seem to be a source of atmospheric CO_2 based on the CO_2 flux at the sea-air interface, the combined effects of the riverine input in the area, oceanic input, depositional export,and microbial carbon pump(DOC conversion and output) indicate that the China Seas represent an important carbon storage area.