湖南地区不同集约化栽培模式下双季稻稻田CH4和N2O的排放规律

采用静态暗箱-气相色谱法研究了湖南双季稻稻田不施氮(NN)、当地常规(FP)、高产高效(YE)、再高产(HY)、再高效(HE)5种不同栽培模式下温室气体(CH4、N2O)的排放规律.结果表明:水稻生长季CH4累积排放量变化为(206.5±37.5) kg· hm-2(FP,早稻)～(490.5±65.7) kg·hm-2(HE,晚稻),N2O-N累积排放量变化为(0.08±0.05) kg·hm-2(NN,早稻)～(0.326±0.15) kg·hm-2(HY,晚稻).不同栽培模式对CH4和N2O的排放都有显著影响(p＜0.05).HE模式CH4排放显著高于其他模式62％～ 87％(p＜0.05),尤其是晚稻季节;除NN模式外,其他4种模式间N2O排放差异不显著.冬季休闲期也是CH4和N2O排放的重要时期,分别占全年排放量的9.7％～19.7％和42％～ 62％.CH4主导了稻田不同栽培模式下的综合温室效应,在各模式中均占95％以上.施氮肥提高了作物产量,降低了温室气体强度(GHGI).在5种模式中,YE和HY模式温室气体强度较小,HY模式下仅为(0.97±0.16) kg·kg-1(以每kg产量排放的CO2当量计).因此,与FP模式相比,YE和HY模式既能提高产量和氮肥利用率,也能减缓温室效应;但HE模式排放的温室气体较高,在实际应用前尚需进一步研究.     

巢湖不同富营养化区域甲烷排放通量与途径

为了更好的认识不同富营养化区域甲烷（CH₄）排放通量及途径的时空异质性,本文以我国典型富营养化浅水湖泊-巢湖为研究对象,设置西北湖湾、西湖心和中湖心3个研究点位,采用漂浮通量箱和经验模型分析等方法对其水-气界面CH₄排放通量与途径进行季节性研究.结果表明水体与沉积物中CH₄溶存浓度、水-气界面CH₄排放通量同水体营养盐水平及叶绿素a含量的空间变化相一致,且均表现为西北湖湾最高,其水体CH₄溶存浓度为（0.178 ±0.002）~（1.123 ±0.026）μmol/L、表层沉积物中CH₄含量为（70.5 ±30.7）~（189 ±97.0）μmol/L、CH₄总排放通量为（50.1 ±2.93）~（1232 ±28.6）μmol/（m²·h）;3个点位的CH₄扩散通量占总排放量的7.3%~42.9%,冒泡通量占57.1%~92.7%,富营养化程度最高的西北湖湾冒泡通量占比最高;CH₄排放通量大小与途径同时受季节变化影响,夏季CH₄冒泡与总排放通量均最高,其中冒泡对总通量的贡献高达98.1%.     

喀斯特小流域河流溶存甲烷浓度时空变化特征

以宜昌境内喀斯特河流下牢溪为研究对象,通过对流域内15个采样点为期1a间隔约2周1次的水量、水质及CH₄浓度同步监测,探讨河流溶存CH₄浓度时空变化规律及影响因素.结果表明：下牢溪溶存CH₄浓度变化范围为0.002~1.492μmol/L,全年平均浓度0.133μmol/L,整体表现为大气CH₄的源.河流溶存CH₄浓度呈现夏秋高、冬春低的变化特征,主要受温度驱动.雨季CH₄浓度受温度和降雨共同调控.温度越高,产生流量稀释效应的降雨量阈值也越大.下牢溪CH₄浓度空间分异性显著,小型拦水坝前浓度最高,最低值出现在河底坡降较大的天然峡谷型河道.人为活动不同程度的提高了相应河段的CH₄浓度水平,是小流域CH₄浓度空间分布格局的重要影响因素.流域CH₄浓度空间分布无明显时间稳定性特征,这可能与陆源输入及水平、垂向输出等动态因素有关,实施全流域采样监测对小型河流碳排放估算十分必要.     

永兴岛大气CH4浓度变化特征及影响因子研究

依托国家海洋局三沙海洋环境监测中心站,基于激光大气温室气体分析仪（GLA331-GGA）,搭建了一套全自动、连续、高精度观测大气CH₄的观测系统.通过气团后向轨迹输送特征,结合数值统计方法（局部近似回归法）,对西沙永兴岛区域2013年12月~2017年11月期间的观测数据进行了数据筛分和分析.结果显示：西沙海域大气CH₄季节变化与北半球大气本底变化状况类似,冬季高、夏季低,年平均增长率约为11.9×10^-9,年平均季节振幅为81.1×10^-9;其日变化呈现中午低、凌晨高的单周期正弦变化特征;该区域风场数据和气团后向轨迹分析表明：季风是影响该区域CH₄浓度变化的最主要因素.     

Land Use and Climate Variability Amplify Carbon,Nutrient, and Contaminant Pulses: A Review with Management Implications

Nonpoint source pollution from agriculture and urbanization is increasing globally at the same time climate extremes have increased in frequency and intensity. We review >200 studies of hydrologic and gaseous fluxes and show how the interaction between land use and climate variability alters magnitude and frequency of carbon, nutrient, and greenhouse gas pulses in watersheds. Agricultural and urban watersheds respond similarly to climate variability due to headwater alteration and loss of ecosystem services to buffer runoff and temperature changes. Organic carbon concentrations/exports increase and organic carbon quality changes with runoff. Nitrogen and phosphorus exports increase during floods (sometimes by an order of magnitude) and decrease during droughts. Relationships between annual runoff and nitrogen and phosphorus exports differ across land use. CH₄ and N₂O pulses in riparian zones/floodplains predominantly increase with: flooding, warming, low oxygen, nutrient enrichment, and organic carbon. CH₄, N₂O, and CO₂ pulses in streams/rivers increase due to similar factors but effects of floods are less known compared to base flow/droughts. Emerging questions include: (1) What factors influence lag times of contaminant pulses in response to extreme events? (2) What drives resistance/resilience to hydrologic and gaseous pulses? We conclude with eight recommendations for managing watershed pulses in response to interactive effects of land use and climate change.     

Analysis of availability and accessibility of hydrogen production: An approach to a sustainable energy system using methane hydrate resources

It is considered that use of hydrogen as an energy source may contribute to environmental improvement and provide an alternative energy system. Moreover, it is anticipated that hydrogen will be in great demand in the near future for use in such vehicles as fuel cell-based cars. Research and development of a number of advanced methods of hydrogen production (OTEC, water photolysis using a semiconductor, a municipal waste gasification—smelting system, etc.) is currently under way.A comparison of different hydrogen-rich fuels in this paper shows that methane is advantageous for hydrogen production from the viewpoint of energy efficiency as measured by thermodynamic analysis. This paper therefore proposes combining existing technology for hydrogen production with an unconventional methane source in order to facilitate the realization of a hydrogen energy system: i.e., this paper proposes combining the process of steam reforming, which is commercialized worldwide, with use of untouched natural gas hydrate (NGH) resources. Gas hydrate deposits, which are distributed worldwide, hold great amounts of methane gas and have hardly been touched. This paper presents the economic parameters of NGH development and discusses the concept of devising useful applications of NGHs, with consideration given to (1) independence from current fossil fuels; (2) energy transport using the hydrate system; (3) CO₂ sequestration — replacement of methane hydrate with CO₂ hydrate in the submarine layer and (4) improvement of current steam reforming of methane by CO₂ reuse and zeolite application. This paper thus proposes a new solution that will make a key contribution to the systematic development of a new sustainable energy structure.Readers should send their comments on this paper to: BhaskarNath@aol.com within 3 months of publication of this issue.     

Ⅱ824^—2综放工作面瓦斯综合治理试验研究

通过对淮北芦岭矿Ⅱ824^-2综放工作面瓦斯综合治理的试验研究，摸索出了高瓦斯综放工作面瓦斯治理的有效方法，取得了较好的瓦斯抽放和通风排放效果。     

DISSOLVED GAS ANALYSIS FOR ASSESSING THE FATE OF NITRATE IN WETLANDS1

ABSTRACT: Dissolved gas analysis permits direct detection of ground water denitrification, a technique we used in this study to assess the fate of nitrate in a riparian wetland. Dissolved argon (Ar) and dinitrogen (N₂) were measured in transects of nested piezometers installed at different depths within upwelling regions of a riparian wetland. The method uses the Ar content in the water as a natural inert tracer for assessing background content of N₂ from the previous air/water equilibrium. Within the wetland under study, anoxic to suboxic ground water became more oxic in piezometers close to the aquifer layer, indicating upwelling of oxic ground water. Assessment of loss of nitrate and Ar in ground water within an upwelling zone indicated that shallow piezometers had significant N₂ loss through degassing. Most of the measured nitrate‐nitrogen (NO₃^?‐N) loss of 205 μM in a piezometer nest could be accounted for by total N₂‐N produced (169 μM N), calculated from changes in dissolved N₂ and estimated N₂ degassed. Degassing due to methane (CH₄) production was also detected in some shallow piezometers within nests. This technique for analysis of dissolved gases in ground water can be applied to detect small changes in N gas concentration and aids in assessing the fate of nitrate along a ground water flow path.     

废铁屑强化污泥厌氧消化产甲烷可行性分析

有关全球气候变化的《巴黎协定》落槌,预示着污水处理追求碳中和运行的时代已经来临.碳中和狭义理解即能源自给自足,这就要求污水处理厂应最大程度转化污水中有机物或产生的剩余污泥所蕴含的有机能源,并将其生成可再生能源——甲烷.然而,剩余污泥能源转化率较低一直都是限制厌氧消化技术广为应用的瓶颈.在污泥预处理技术之外,向厌氧消化系统中投加废铁屑强化甲烷生产有望成为另一个提高能源转化率的突破口,继而实现"以废促能、变废为宝"的目的.本综述从铁腐蚀析氢现象入手,在描述铁腐蚀析氢原理、析出H2对产CH4过程影响的基础上,对铁在厌氧系统ORP减少方面的作用、对厌氧微生物生理、生化特性的影响、对涉及微生物酶活的影响等进行了全面的介绍.最后,还通过生命周期评估(LCA)评价了基于废铁屑的污泥厌氧消化技术对环境的影响及经济合理性.     

含NaCl超细水雾抑制甲烷爆炸实验研究

为研究含NaCl添加剂超细水雾对甲烷爆炸的影响,在自制的半封闭透明管道内,进行含NaCl添加剂超细水雾抑制甲烷爆炸试验,通过检测和分析在不同NaCl浓度情况下超细水雾的粒径和甲烷爆炸的平均火焰传播速度、爆炸超压以及平均升压速率,探究NaCl浓度对超细水雾粒径及其对抑制甲烷爆炸有效性的影响。研究结果表明:NaCl浓度对超细水雾粒径影响较小;对于体积分数为9.5%的甲烷,相比于纯甲烷爆炸,其平均火焰传播速率、最大爆炸超压以及平均升压速率分别下降了53.7%,63.4%和60.7%,相比于超细纯水雾,其平均火焰传播速率、最大爆炸超压以及平均升压速率分别下降了38.6%,58%,56%;在通雾量相同的条件下,浓度为2.5%NaCl超细水雾对体积分数为9.5%的甲烷爆炸抑制性能最佳;含NaCl添加剂超细水雾的物理化学共同作用可以有效抑爆甲烷。