CHEMISTRY OF COALBED METHANE DISCHARGE WATER INTERACTING WITH SEMI‐ARID EPHEMERAL STREAM CHANNELS1

ABSTRACT: The objective of this study was to examine the chemistry of Coalbed Methane (CBM) discharge water reacting with semi‐arid ephemeral stream channels in the Powder River Basin, Wyoming. The study area consisted of two ephemeral streams: Burger Draw and Sue Draw. These streams are tributaries to the perennial Powder River. Samples were collected bimonthly from three CBM discharge points and seven channel locations in Burger Draw and Sue Draw. Samples were also collected bimonthly from the Powder River above and below the confluence of Burger Draw. Before sample collection, the pH and electrical conductivity (EC) were measured in the field. Samples were transported to the laboratory and analyzed for alkalinity, major cations, and anions. From the measurement of sodium (Na), calcium (Ca), and magnesium (Mg), practical sodium adsorption ratio (SARp) and true sodium adsorption ratio (SARt) were calculated. Results suggest pH and EC of CBM discharge water was 7.1 and 4.3 dS/m, respectively. The CBM discharge water consisted of higher concentrations of sodium and alkalinity compared to other components. The pH of CBM discharge water increased significantly (p = 0.000) in the downstream channel of Burger Draw from 7.1 to 8.84 before it joined with the Powder River. Dissolved calcium concentration of CBM discharge water decreased significantly (p = 0.000) in the downstream channel water. Subsequently, SARp increased approximately from 24 to 29. The SARt also increased significantly (p = 0.001) in the downstream channel water. For instance, SARt of CBM discharge water increased from 32.93 to 45.5 downstream channels after the confluence of Sue Draw with the Burger Draw. The only significant difference in water chemistry above and below the confluence of Burger Draw with the Powder River was pH, which increased from 8.36 to 8.52. The significant increase in SAR values of CBM discharge water in Burger Draw and Sue Draw tributaries suggest a careful monitoring of salinity and sodicity is needed if CBM discharge water is used for irrigation in semi‐arid environments. Results discussed in this study will be useful to downstream water users who depend on water for irrigation.     

蔬菜类废弃物甲烷发酵的产气潜能及过程特征

蔬菜废弃物具有适合厌氧发酵的特性。采用Batch实验方法,对5种常见的蔬菜废弃物的产气潜能进行研究,并在此基础上进一步对厌氧发酵过程限制性步骤及物质转化特征进行分析。研究结果表明:5种蔬菜废弃物累积产甲烷量在发酵0～10 d内增加较快,土豆和白菜废弃物产甲烷潜能最大,分别达到102 mL·g-1(VS),和83 mL·g-1(VS),而黄瓜废弃物的甲烷化潜能较低,只有35 mL·g-1(VS)左右。动力学参数拟合表明:土豆和白菜废弃物厌氧发酵水解、酸化、乙酸化和甲烷化各过程转化速率都明显高于其他废弃物,并且各过程最大转化潜能也较其他类蔬菜高出2倍之多。厌氧发酵限制性步骤分析表明,快速水解生成的SCOD不能有效地转化为VFAs,限制了白菜废弃物厌氧消化的后续转化,而VFAs的累积则是胡萝卜、黄瓜和土豆废弃物厌氧发酵的限制性步骤, SCOD以及VFAs同时累积是茄子废弃物发酵过程的显著特征。对各物质发酵过程物质转化特征分析表明,各废弃物由于4 d以后甲烷菌对乙酸的利用减慢,导致丙酸向乙酸的转化减慢而发生累积现象,10 d以后由于产酸过程的减弱,累积的丙酸盐逐渐转化。     

油气处理场站温室气体甲烷排放特征与量化

油气生产过程是甲烷重点排放源,对气候变化产生显著影响。采用便携式火焰离子检测器 (FID) 和Hi-Flow大流量仪等设备,对我国某油田3座油气处理场站甲烷泄漏排放特征进行了研究,明确了组件泄漏率,量化了重点源项甲烷排放速率,构建了设备设施甲烷排放因子,开展了甲烷排放量核算并提出了管控建议。结果表明,该油田油气处理场站设备组件与管线的甲烷泄漏率为0.7%~1.2%,压力表、阀门和储罐等在泄漏源项中占比较高。不同类型泄漏组件甲烷排放速率具有显著差异,处理场站的甲烷排放速率为111.66~274.63 L·min⁻¹。单个储罐和场站的甲烷排放因子分别为989.9 L·h⁻¹和0.19 L·m⁻³。3座场站年度甲烷排放量为303 783.40 m³,储罐是首要排放源,对总排放量贡献占比为94.1%。组件泄漏导致的甲烷排放主要源于高强度排放源,15%的泄漏点贡献了排放量的88.4%。该研究结果可为油田油气处理场站泄漏防控和温室气体排放控制提供参考。     

粉煤灰、炉渣提高生物反应器垃圾处理性能研究

通过粉煤灰、炉渣和生活垃圾共置处理,研究粉煤灰、炉渣提高生物反应器垃圾处理性能的机理和效果。结果表明:粉煤灰、炉渣可以有效去除重金属离子,调节反应器内pH,使渗滤液停留时间延长4倍～5倍,产气量提高5.9倍～7.8倍,甲烷含量可提高2倍以上,共置处理效果显著好于生活垃圾单一处理。     

硫酸根对有机废水厌氧生物处理的影响

利用连续流上流式厌氧污泥床在控制和不控制H_2S浓度两种情况下,考察SO_4~(2-)对有机物厌氧生物处理的影响。试验表明,硫酸根本身对厌氧处理没有毒害作用,它对厌氧处理过程的破坏主要是其还原产物H_2S造成的。在用Fe~(2+)控制H_2S的情况下,硫酸根的存在和浓度大小对出水TOC、TOC去除率、产气量、气化率无不利影响,但会使气体中甲烷含量及甲烷产率逐渐减小而二氧化碳含量及二氧化碳产率逐渐增大,     

Ⅰ Ⅱ-ASBR中厌氧颗粒污泥的微生物组成及特性

在35℃下以奶粉人工合成废水为底物连续运行了两段厌氧反应器(ⅠⅡ-ASBR),且于ⅠⅡ两柱中形成了两种不同的厌氧颗粒污泥,为了解厌氧颗粒污泥的微生态结构及生物学特性,对ⅠⅡ两柱中厌氧颗粒污泥的形态及微生物组成进行扫描电镜观察,并测定了其不同基质中的比产甲烷活性、辅酶F420和胞外多聚物的含量。结果表明:ⅠⅡ-ASBR反应器ⅠⅡ两柱中厌氧颗粒污泥形态及微生物组成差异明显,Ⅰ柱的厌氧颗粒污泥大而密实,Ⅱ柱的较小,呈多孔的网状结构,Ⅰ柱中厌氧颗粒污泥以甲烷八叠球菌、球菌及短杆菌为主,丝状菌较少,Ⅱ柱则以丝状菌、短杆菌为主,球菌较少;Ⅰ柱颗粒污泥利用葡萄糖、甲酸、丙酸的产甲烷活性较高,利用乙酸的活性相对较低,Ⅱ柱颗粒污泥利用葡萄糖、乙酸的产甲烷活性较高,而利用甲酸、丙酸的产甲烷活性较低;辅酶F420的含量Ⅱ柱比Ⅰ柱明显要高,而胞外多聚物含量Ⅰ柱比Ⅱ柱的高。     

硝酸盐对矿化垃圾中兼/厌氧甲烷氧化的影响

设计全因子实验研究了NO-3-N对填埋10~12 a的矿化垃圾中兼/厌氧甲烷氧化作用的影响.结果表明,兼/厌氧条件下,NO-3-N能促进矿化垃圾中CH4的去除.初始CH4和NO-3-N对CH4去除和N2产生有明显影响,且两者具有交互作用(P<0.05).CH4去除量随着初始CH4体积分数的增加而增加,添加一定含量的NO-3-N能促进CH4去除,同时通入一定体积分数CH4可以明显促进反硝化作用,说明矿化垃圾中NO-3-N还原能与兼/厌氧甲烷氧化耦合.本实验条件下,初始CH4体积分数为30%,NO-3-N含量为110 mg·kg-1时耦合效应较好.     

三江平原小叶章湿草甸CH4地-气交换特征

用密闭不透明箱-气相色谱法对三江平原小叶章湿草甸进行了为期2 a的现场观测研究.结果表明三江平原季节性积水的小叶章湿草甸全年CH4排放呈明显的双峰型变化.在非冰冻期(5月至10月)CH4排放通量为0.297～18.914 mg·m-2·h-1, 排放峰值出现在6月和8月、9月;冰冻期(11月至次年4月)CH4排放通量为0.048～2.921 mg·m-2·h-1, 排放低值出现在冬季的12月至次年3月之间,以及发生季节性干旱的7月.冰雪覆盖下的小叶章湿地依然有CH4排放,冰冻期CH4排放量约占全年排放总量的4.94%.在季节性积水或过湿的环境中,小叶章湿草甸CH4排放通量的季节变化主要由温度和土壤水分条件共同控制,其日变化特征表现为白天排放通量大,夜间则小.     

Methanotrophic community structure of aged refuse and its capability for methane bio-oxidation

Aged refuse from waste landfills closed for eight years was examined and found to contain rich methanotrophs capable of biooxidation for methane. Specially, community structure and methane oxidation capability of methanotrophs in the aged refuse were studied. The amount of methanotrophs ranged 61.97 103–632.91 103 cells/g (in dry basis) in aged refuse from Shanghai Laogang Landfill. Type I and II methanotrophs were found in the aged refuse in the presence of sterilized sewage sludge and only Type I methanotrophs were detected in the presence of nitrate minimal salt medium (NMS). The clone sequences of the pmoA gene obtained from the aged refuse were similar to the pmoA gene of Methylobacter, Methylocaldum, and Methylocystis, and two clones were distinct with known genera of Type I methanotrophs according to phylogenetic analysis. Aged refuse enriched with NMS was used for methane biological oxidation and over 93% conversions were obtained.     

提高煤层气采收率的CO2埋存技术

作为常规油气重要接替补充的非常规天然气,煤层气越来越受到世人的关注.如何提高煤层气采收率是摆在煤层气开发工程师面前迫切需要解决的技术难题.通过向煤层中注入CO2,既可以提高煤层气采收率又能间接地实现CO2减排,即提高煤层气采收率的CO2埋存技术(CO2-ECBM).该项技术已在世界各地迅速发展,并取得一些实质性进展.文...