密植浒苔对冬季露天池塘池底水温、酸碱度和溶解氧的影响效应

借助环境数据实时采集装置,于2014年1月5日至1月22日连续开展了冬季露天池塘培植浒苔对池底水温、酸碱度和溶解氧的实时监测工作。结果表明：（1）密植浒苔可在不改变池底水温峰值期时辰数的基础上,提前1个时辰到达峰值,在不影响到达谷底时辰的同时,使低谷期缩短了1个时辰,并由此延长了水温由峰到谷的转换时长;（2）密植浒苔可保持池底p H值的基本稳定,并在不改变池底p H值时段变化节律的基础上,使日均p H值由9.3下调至8.6;（3）密植浒苔在对池底DO值的时序变化影响上与池底水温相仿,并使日均DO值由10.61mg/L下调至6.80mg/L。     

海蜇螅状幼体和碟状幼体窒息点和耗氧量的初步测定

在温度２０±１℃和盐度２２─２４‰条件下，对海蜇螅状幼体和碟状幼体进行了窒息点和耗氧量的初步测定。结果表明：螅状幼体的窒息点低于０．１０ｍｇ·Ｌ，直径３．４─１０．２ｍｍ碟状幼体的窒息点为０．１７─０．２０ｍｇ·Ｌ。螅状幼体的个体耗氧量为２．９３μｇ·ｄ，耗氧率为２．６６ｍｇ·ｇ·ｈ（干重）：直径３．４、４．６和１０．２ｍｍ碟状幼体的个体耗氧量分别为４．７７、２５．４１和７９．４５μｇ·ｄ，耗氧率分别为４．９７、２．４６和１．１２ｍｇ·ｇ·ｈ（干重）。     

基于模糊神经网络的池塘溶解氧预测模型

在分析了池塘溶解氧影响因素的基础上，利用模糊神经网络良好的非线性逼近能力建立了池塘溶解氧的模糊神经网络预测模型。神经网络模型如采用常规的BP或其它梯度算法，常导致训练时间较长且易陷入局部极小点，本实验采用快速的粒子群优化算法对模糊神经网络进行训练，收敛速度明显加快。实验结果表明采用该方法预报溶解氧的预测精度较常规BP递推算法的预测精度明显提高，所采用的模型能对溶解氧进行可靠的预测，该方法为研制开发智能水质检测仪以及工厂化养殖工作奠定了基础，对实际生产具有一定的指导意义。     

Dynamics of dissolved oxygen (DO) in ponded water of a paddy field

The transfer of heat and dissolved oxygen (DO) through water is important to understand the phenomenon of ponded water in a paddy soil. The heat from solar radiation is absorbed at the soil surface and transferred into the ponded water by convection. This study clarified the dynamics of DO, as well as the role of convection in water in DO transfer in the ponded water of a paddy field. DO concentration in the ponded water of a paddy field was measured in situ in the daytime and during the night. The results were confirmed in lab-scale model experiments. The DO concentration and temperature profiles in the ponded water of a lab-scale paddy field model were investigated under convective and non-convective conditions using solar radiation and infrared radiation, respectively. Under the ponded condition, solar radiation was absorbed at the soil surface whereas infrared radiation was absorbed at the water surface and thereby convective and non-convective conditions were generated, respectively. The diurnal variation in DO concentration was closely related to the intensity of solar radiation. Oxygen generation by micro-algae and its subsequent circulation by convection resulted in uniform DO concentration profiles, with super-saturated values in the ponded water in the daytime. Eventually oxygen was released to the atmosphere by deaeration until DO in water was depleted to the saturated level. During the night the oxygen moved from the atmosphere into the water surface by reaeration which depends on the oxygen deficit related to saturation. The oxygen deficit is caused by the respiration of microorganisms. The oxygen, that moved from the atmosphere to the water surface, was transferred to the soil surface by convection in the water layer. Thus convection plays an important role in the DO transfer in the ponded water of a paddy field. The DO dynamics is correlated with biological processes in the ponded paddy soil.     

Nutrient-flow wick culture system for potted plant production: System characteristics and plant growth

To compliment the current subirrigation systems used for production of potted plants, a nutrient-flow wick culture (NFW) system was developed and compared with other subirrigation systems, such as an ebb and flow culture (EBB) system and a nutrient-stagnant wick culture (NSW) system in relation to their system characteristics and plant growth. Kalanchoe (Kalanchoe blossfeldiana cv. New Alter) was cultivated in a 6 cm pot for 10 weeks in each subirrigation system. The water-absorption pattern of the medium, water content of the medium, water loss, algal growth, salt-buildup and plant growth under various culture systems were observed. The water contents of medium under the NFW and EBB systems showed fluctuations from 30 to 40% and from 50 to 60% (by volume), respectively, whereas the water content under the NSW system gradually increased to over 40% without fluctuation. Relative to other systems, the water loss in the NFW system was 50–70% due to the reduction in the evaporation from the surfaces of the trough and medium. Algae appeared in the NSW system because the nutrient solution was always stagnant in the trough, while it was not observed under the NFW system. The dissolved oxygen in the nutrient solution was the highest during the irrigation period and the salinity in the medium was the lowest in the NFW system. With regard to system characteristics, the NFW system was simple, water-saving and efficient. In addition, the growth of kalanchoes in the NFW system was similar to those in the NSW and EBB systems at an irrigation frequency of five times a day.     

不同氨氮和溶解氧条件下循环海水养殖系统生物滤池对氨氮、化学耗氧量及颗粒悬浮物的处理效果

为了建立优化的循环海水养殖系统,采用水质国标检测方法分析了珊瑚石生物滤池在不同氨氮和溶解氧(DO)负荷实验条件下对养殖废水中氨氮、化学耗氧量(COD)及颗粒悬浮物(SS)的处理效果。结果显示,进水氨氮浓度对出水氨氮(正相关)、COD(正相关)均有极显著的影响(P0.01),对SS处理效果影响不显著。当进水氨氮浓度为0.45~0.65 mg/L时,滤池对水体处理效果最优(氨氮平均清除率为82.1%±3.3%;COD平均清除率为7.1%±1.5%;SS平均清除率为5.8%±1.6%)。DO浓度对水体氨氮(负相关)和COD(负相关)处理效果的影响显著(P0.05),对SS处理效果影响不显著。DO浓度为5.0~7.0 mg/L时,水体处理效果最优(氨氮平均清除率为78.7%±3.5%;COD平均清除率为23.0%±5.3%;SS平均清除率为7.1%±2.0%)。因此,本实验环境下的循环海水养殖系统珊瑚石生物滤池在氨氮浓度为0.45~0.65 mg/L,DO浓度为5.0~7.0 mg/L时,对水体中的氨氮、COD、SS的综合处理效果最优。     

基于ARIMA模型的湘江流域DO和NH4+–N含量贝叶斯预测

为实时把控湘江流域水质的变化趋势,采用污染比较严重的湘江流域长沙段和益阳段水质指标溶解氧(DO)和氨氮(NH_4~+-N)含量的监测数据,用贝叶斯方法推断经典的ARIMA时间序列模型,并用马尔可夫链蒙特卡罗(MCMC)模拟方法对DO和NH_4~+-N含量进行贝叶斯预测。结果表明,该模型的贝叶斯预测能实现对湘江流域长沙段和益阳段水质指标DO和NH_4~+-N含量的精确点预测、区间预测和概率预测。     

自动增氧型人工湿地对废水中COD的去除效果

针对常规人工湿地中溶解氧不足的问题,采用页岩空心砖构建自动增氧型人工湿地系统,研究构建系统对废水COD的净化效果。结果表明,自动增氧型湿地内的DO比人工强化曝气型湿地高0.1 mg/L左右,COD去除率达到85%以上,比人工曝气型湿地高2%左右。这说明构建的自动增氧系统可提高湿地系统内部供氧能力,提高湿地系统对废水COD的净化效率。     

曝气生物滤池工艺处理港区污水中脱氮关键控制因素研究

[目的]探讨曝气生物滤池在处理港区污水中反应器的最佳工况参数.[方法]以某城市港区污水为处理对象,通过改变反应器的工艺参数,包括进水COD浓度、水力停留时间（HRT）和溶解氧（DO）等,考察各因素对反应器脱氮效果的影响,并综合考虑经济性原则,寻求最优化的工艺参数.[结果]进水COD浓度为190～220 mg/L时,有利于反硝化作用和TN的去除.HRT的延长有助于系统内硝化菌群的代谢,当HRT为6h时,NH4＋-N、TN去除率可维持较高水平.DO浓度宜保持在2.5～3.5 mg/L,可保证出水稳定的前提下尽量降低DO值,以使反应器能耗降低.[结论]该研究为港区污水的处理提供了一种新方法.     

桑沟湾养殖海带(Sacharina japonica)碎屑降解速率及影响因素

通过实验室可控条件,以桑沟湾(Sanggou Bay)养殖海带(Sacharina japonica)为研究对象,探讨养殖海带碎屑降解过程中营养盐释放速率及对底质、溶解氧的影响.实验设置2个底质条件(加底泥,无底泥)、2个溶氧条件(好氧,厌氧),各处理组设3个平行,实验持续27 d.结果显示,(1)加入底泥,可以促进海带碎屑的降解.实验结束时,加入底泥组无机氮(DIN)、总氮(TN)、活性磷酸盐(DIP)、总磷(TP)的平均释放速率分别为1.234、1.802、0.028、0.033 μmo1/(g.d),显著高于未加底泥组的0.039、1.476、0.005、0.010 μmo1/(g·d).而未加底泥组的可溶性有机氮(DON)释放速率为1.437 μmo1/(g·d),显著高于底泥组的0.568 μmo1/(g.d).(2)厌氧条件有利于海带碎屑中P的降解释放,释放的TP中以可溶性有机磷(DOP)为主.TP、DIP、DOP的降解速率显著高于非厌氧条件.但是,厌氧条件下无机氮释放速率为0.097 μmo1/(g·d),仅为好氧条件下无机氮的8％,而总氮为好氧条件下的71％.(3)底泥的加入显著提高了水体的N:P,达到207.83±301.37,厌氧状态使水体N:P降低到9.38±6.55,都较大的偏离对照组的16.82±1.26,远远偏离经典Redfield值(16∶1).整个实验说明养殖海带降解过程受底质、溶氧条件影响,同时,大量海带碎屑腐烂降解,将会对养殖系统的营养盐浓度及结构产生影响.