规模化牲畜养殖场的环境效应及其对策

通过对江苏省2个典型地区的4个生猪养殖场的饲料、牲畜排泄物、土壤、地表水及水土水中养分状况的调查采样与分析，对牲畜规模养殖的环境效应进行了评价。在此基础上，对牲畜养殖排泄物的养分管理与资源化利用提出了建议，并通过对牲畜排泄物中养分状况及作物养分需求状况的分析统计，提出了种植－养殖区域养分平衡管理模式。     

河流水质1号模型探讨

介绍了河流水质模型70年来的发展历程和目前存在的不足之处,论述了河流水质1号模型(RwQM1)的研究成果.河流水质1号模型从活性污泥模型ASM中发展而来,并推出了建立模型的决策化方法,其对生化反应模型的完善而成为河流水质模型发展的一个标准平台.本文重点介绍了其在生化反应模型方面的进展,并和QUAL2E做了比较.     

污水生物处理单元平衡分析方法研究(Ⅰ)

依据热力学第二定律建立了污水处理单元Yong平衡分析的灰箱模型，提出了进行处理单元过程Yong评价的指标体系．在热力学意义上，污水生物处理是通过微生物内部的Yong耗散来消耗污水污染物能量的过程，推动该过程加速进行需要耗费外部的Yong．因此，节能的主要目的是节Yong，即应防止推动力过剩造成反应器单元的外部Yong损失．这一方法体系将为合理科学评判处理过程能耗机制奠定重要的理论基础．     

水解池—稳定塘工艺越冬技术措施研究

为提高污水稳定塘在冬季的处理效果,用水解池作为预处理措施,以降低有机负荷并改善污水的可生物降解性,因而提高了低温条件下的降解速率.通过对系统的热量平衡分析和技术经济分析,研究采用塑料大棚减慢稳定塘热量散失的措施.结合研究其它一些强化措施,提出了能适合北方地区冬季气候特点的稳定塘工艺流程.     

华北平原的水土资源平衡研究

采用精确的水土资源平衡计算模型 ,辅以田间观测资料 ,分析计算了华北平原农业水资源量与作物需水量之间的平衡问题。结果显示 :在充分供水的条件下 ,本区农田 (884.8万hm₂)需水量为744.36亿m3,相应的作物亏水量为309.37亿m3,有效灌溉面积 (653.2万hm₂)上的亏水量为228.73亿m3;而1995年水利工程提供的农业总用水量已达261.78亿m3,但仍有116.16亿m3的亏水量 ;文中同时对评价区内农田的有效降水量、灌溉水的田间利用量、毛管上升水量等进行估算。指出 ,虽然冬小麦的平均水分满足率为82 % ,但关键期的水分满足率 (64 % )仍然制约粮食产量的增长 ,设想通过提高渠系利用系数和优化灌溉等措施 ,华北平原的农业可望达到水土资源平衡利用的状态     

城市垃圾焚烧发电系统热平衡分析与优化方案

以城市垃圾焚烧过程的热工计算为基础，深入研究了热平衡分析与能量回收之间的关系。针对国内在垃圾焚烧发电领域存在的主要问题，提出了传统工艺的优化方案，并对我国城市垃圾焚烧发电的能量回收利用前景进行了预测分析。     

城市绿化树木碳氧平衡效应研究

本文通过实测广州市内几种常见绿化树木的光合强度和呼吸强度以及叶面积指数，计算城市绿地吸收二氧化碳和释放氧气的能力。得出各种树木的叶片光合强度。由于各树木的叶面积指数不同，绿地的吸碳放氧能力也不同。据此，从人类呼吸的基本需要考虑，探讨了城市地定额指标问题。     

活性污泥数学模型中异养菌产率系数测定方法的研究

采用间歇活性污泥法和呼吸计量法测定活性污泥数学模型中异养菌产率系数.研究结果表明,间歇活性污泥法测定结果受试验控制条件特别是污泥有机负荷的影响非常大,且试验周期比较长;人工配水条件下,呼吸计量法测定异氧菌产率系数(YH)在0.71以上,比活性污泥数学模型推荐值高,其结果与底物性质有关,该方法准确性高,重现性良好.     

新型堆肥装置设计及其应用研究

根据城市生活垃圾的特点和性质,利用物料平衡和热力学原理进行好氧堆肥实验装置的设计,并对堆肥发酵仓容积的确定和配套辅助设备进行了研究,得出当堆肥装置直径小于225m时,需采取保温措施。通过强制通风静态仓式堆肥小试实验进行的城市生活垃圾堆肥结果表明,通过30℃及以上的水浴加热,可实现固体废物的堆肥化。     

S–O–C isotopic picture of sulphate–methane–carbonate system in freshwater lakes from Poland. A review

Microbial oxidation of organic compounds (including methane), in freshwater sediments, may result in precipitation of carbonates, which may become an important geochemical archive of paleoenvironmental variations. Most probably low δ¹³C value in calcite in eutrophic systems results from an advanced oxidation of organic compounds in turbulent or/and sulphate-rich conditions. Likewise, high δ¹³C value in calcite from organic-rich sediments may evidence low redox potential of the freshwater system. Oxidation of methane and organic matter results in significant isotope effects in sulphates dissolved in water. Therefore, to better understand the origin of carbon isotope signal in carbonates, concentration and stable isotope measurements in dissolved sulphate (water column), bubble methane and calcite (freshwater sediments) have been carried out in 24 lakes, 2 ponds and 4 rivers in Poland. The highest concentration of sulphate has been detected in rivers (85.47 SO₄ ²⁻ mg/l) and an artificial lake (70.30 SO₄ ²⁻ mg/l) located in the extremely SO₄ ²⁻-polluted region called the “Black Triangle”. The lowest concentration of sulphate is found in dystrophic and mountain lakes (from 0.5 SO₄ ²⁻ to about 3 mg/l). The lowest δ³⁴S(SO₄ ²⁻) and δ¹⁸O(SO₄ ²⁻) values occur in unpolluted lakes in eastern Poland (−0.94 and 1.38‰, respectively). The highest S and O isotopic ratios are found in a polluted lake in western Poland (δ¹⁴S(SO₄ ²)=12.95‰) and in a dystrophic lake in eastern Poland (δ¹⁸O(SO₄ ²) = 16.15‰) respectively. It is proposed that δ³⁴SO₄ ²⁻ and (¹⁸O(SO₄ ²⁻) values in lakes represent a good tool to assess and quantify anthropogenic impact by acid precipitation and to monitor variations in the trophic state and redox processes controlled by biodegradation of organic compounds in sediments and water column. In general, increasing depth (up to 12 m) of the water column is associated with decreasing trend the δ¹³C(CH₄) value from about –35 to about –78‰. However, δ¹³C value in sedimentary calcite (δ¹³C vary from –10 to 0.5‰) shows opposite trends as compared to the corresponding methane. This is probably due to redox processes and distribution of heavy isotopes between methane and calcite. Likewise, turbulent water (river) show high δ¹³C value in methane and low δ¹³C value in calcite—this is probably due to an enhanced oxidation of methane producing ¹³C-depleted CO₂. In contrast to clean lakes, it is observed that an increase of the δ¹³C(CH₄) value occurs with increasing depth of the water column in a strongly SO₄ ²⁻-contaminated lake. This is probably due to a loss of biological buffering potential of the lake accompanied by an active oxidation of methane precursors.