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961.
Deborah Ulinski Potter Michael P. Stevens Judy L. Meyer 《Journal of the American Water Resources Association》1982,18(4):627-633
ABSTRACT: Information on biologically important physical and chemical variables is presented for Lake Oconee, a newly impounded pumped storage reservoir in Georgia. During its first summer, when no pumping occurred, temperature, oxygen, pH, inorganic nitrogen, and phosphorus were vertically stratified with severe hypolimnetic oxygen depletion. During the second summer, when pumped storage was in operation, more homogenous vertical profiles, generally higher oxygen, and lower dissolved nutrient concentrations were observed. These pumped storage effects were observed at all stations, rather than being confined to the immediate vicinity of the dam. 相似文献
962.
Jerald L. Schnoor E. Gus Fruh 《Journal of the American Water Resources Association》1979,15(2):506-518
ABSTRACT: A vertical dissolved oxygen model was calibrated and verified using independent field data sets from 1972 and 1973 in Lake Lyndon B. Johnson (LBJ), a short detention time reservoir with anaerobic hypolimnion. Ammonia, carbonaceous BOD, conductivity, and temperature were also simulated as state variables. The conductivity results provided a check on the mass balance and the method of entering the inflows to the reservoir model. Emphasis was placed on calculating the sinks of dissolved oxygen in the hypolimnion which could be useful in management decisions. 相似文献
963.
Stable isotope (18O–H2O, 2H–H2O 34S–SO4
2-) andhydrochemical data (SO4
2-, Fe-concentrations) have beenused to estimate the annual groundwater inflow and outflow of mining lake ML 111 and to calculate the total amount of dissolvedsulfate and iron that is carried into the lake by groundwater. The hydrological balance suggests an annual groundwater inflow of 23 700 m3 and an annual groundwater outflow of 15 700 m3. The calculation of the sulfur and iron balances yielded an annual sulfate input of 37 800 kg and an annual iron input of 7000 kg with the groundwater inflow. Furthermore it was shown that significant fluxes of these elements go into the lake sediments which results in continuous release of acidity in the lake water. 相似文献
964.
Films of whey protein and chitosan acetic acid salt have lower oxygen permeability than, for example, ethylene-co-vinylalcohol under dry conditions, but water and water vapor seriously impair the gas barrier properties. To reduce the oxygen permeability at 90% relative humidity and the water-vapor transmission rate at 100% relative humidity, the films were coated with an alkyd, a beeswax compound, or a nitrocellulose lacquer. Permeability and transmission rate measurements were performed in accordance with standard methods and showed that the beeswax compound and the nitrocellulose were appropriate as water-vapor barriers. Overall migration to water was measured after 10 days exposure time, with the coated surface exposed to the water, showing that the alkyd-coated and the nitrocellulose-coated films were both below the safety limit for food contact. Water absorbency tests, performed by the Cobb method, showed that the films coated with the beeswax compound or with nitrocellulose lacquer exhibit lower absorbency than the alkyd-coated films. 相似文献
965.
966.
厨余垃圾堆肥蓬松剂技术研究 总被引:13,自引:0,他引:13
为解决厨余垃圾好氧堆肥过程中含水率高、有机物含量大等问题,分别添加锯末、树叶、秸杆和干马粪为蓬松剂进行厨余堆肥技术研究。采用翻转式堆肥设备,利用出口气体检测仪、温度计及扫描电镜,研究添加蓬松剂堆肥过程中耗氧速率,温度,出口CO2、H2S、O2浓度,堆料结构及微生物群落变化。试验结果表明,添加蓬松剂堆肥,堆料所能达到的高温及其停留时间、好氧速率、产CO2气体能力均明显优于对照组,并能很好地控制出口H2S气体浓度。特别是以干马粪和锯末作为蓬松剂,可明显改善堆料孔隙率,吸收多余水分,加速氧和有机物的传输速率,改善好氧堆肥微环境。因此,厨余垃圾堆肥过程中加入干马粪、锯末等蓬松剂是保证堆肥顺利进行、提高堆肥效率的有效方法。 相似文献
967.
详细介绍了战斗机飞行员新型YM9915加压供氧面罩和TK - 11飞行保护头盔配套的高空供氧防护性能生理评价实验结果。分析讨论了新型加压供氧面罩与飞行保护头盔配套的供氧防护性能特点 ,并针对其不足提出改进建议 相似文献
968.
969.
污水处理中影响微孔曝气充氧性能因素的研究 总被引:2,自引:0,他引:2
对污水处理中微孔曝气充氧性能影响因素的研究是一个复杂而又重要的问题。本文对污水水质、曝气器通气量、曝气池运行负荷和方式等几个主要因素对微孔曝气充氧性能的影响进行了研究探讨。鉴于曝气系统能耗在污水处理厂中所占比重较大,加强对该问题的研究,以降低处理厂能耗,有较好的经济意义。 相似文献
970.
Anf H. Ziadat Bruce W. Berdanier 《Journal of the American Water Resources Association》2004,40(3):631-638
ABSTRACT: Ninety‐one sediment oxygen demand (SOD) samples from six designated sites along the stretch of Lower Rapid Creek, South Dakota, were conducted using an in‐situ SOD chamber. Inside the chamber, readings of dissolved oxygen (DO), water temperature, pH, and specific conductance were recorded every minute for more than one hour using the Datasonde 3 Hydrolab. Initial readings of such parameters were recorded for the overlaying water before the deployment of the SOD chamber. Characteristics of the stream conditions, air temperature, barometric pressure, average flow velocity of the stream, depth of the stream, and the flow velocity by the chamber were recorded. Single and multiple linear regression analyses on all parameters indicated that the velocity of the stream is the least critical parameter for SOD in shallow streams. 相似文献