上海黄浦江两支流河流甲烷含量研究

甲烷是一种重要的温室气体,虽然目前大气中含量远小于二氧化碳,但排放增长率却大于后者.研究区域为上海市黄浦江支流苏州河和淀浦河,通过实验数据对比城郊春夏的甲烷排放的差异,探讨甲烷产生的机制及其与环境因子的关系,这将有助于研究河流甲烷排放对于环境变化的影响.研究结果认为河流甲烷主要来源于水中沉积物,其产生与水质、温度等因素相关;同时甲烷摩尔浓度与硝酸根离子质量体积比存在负相关性,与铵根离子质量体积比和有机碳质量分数存在正相关性.     

阳高县沼气池建设的实践

从规划、标准、质量、管护、政策扶持和市场运作等方面介绍了阳高县沼气池建设的实践。     

煤与瓦斯突出预报的模糊聚类关联分析法

首先采用模糊聚类分析对煤与瓦斯突出的样本集合进行分类，建立不同突出程度的模糊模式。然后用关联分析确定待预报样本与模式的关联程度，以此预测预报样本的煤与瓦斯突出危险程度。这种预报方法相对于模糊聚类分类后，将模式与待预报样本组成新的样本集合，再进行聚类分析，以此分类结果进行预报法。不仅可靠程度高，而且能定量描述待报样本与模式的亲和程度。     

规模化牧场开发沼气发电效益好

沼气利用在我国目前多作生活燃能,用于发电的还很少,而且能真正坚持下去的成功报导也不多.本文介绍下(土布)畜牧场4年多来的沼气发电的成功经验,旨在有助于推动规模化畜牧场在沼气能源方面的开发利用,以获取更多、更好的经济、社会、环境的综合效益.     

沼气在果菜粮贮藏业上的应用

文中介绍沼气这种新型绿色能源在果菜粮贮藏中的应用情况,详尽描述了其在贮藏果品、蔬菜中的应用过程,文中对其作用的原理和益处也给予了适当介绍。     

A model for carbon isotope distribution of methane during diagenesis

The evolution of methane carbon isotope with depth has been discussed based on diagenetic reaction kinetics and isotopic Rayleigh fractionational theory. A mathematical model to describe data of methane carbon isotope for the Liaohe oil field has been established.     

Mo/CuZSM-5的微波辐射法制备及其性能研究

借助微波辐射，制备出一系列具有不同Cu^2＋交换度的Mo／CuZSM-5催化剂，并探讨了交换液浓度、固液比、微波强度以及微波加热时间对交换度的影响．研究了不同交换方法、不同交换度下的催化剂对甲烷无氧芳构化反应的催化效果，并进一步对反应条件进行了优化．实验结果表明：交换液浓度和固液比对交换度有较大的影响；与室温离子交换法相比，微波辐射下的离子交换速率和交换度大幅度提高．对不同催化刺样品催化性能的研究结果表明：催化活性与Cu^2＋含量密切相关，Cu^2＋的适量引入有助于提高催化剂的活性和稳定性。红外光谱、X射线衍射测试结果表明：微波辐射离子交换并未改变分子筛载体的结构；Cu^2＋的引入促使更多的活性物种分布在催化剂外表面。     

利用“球壳失稳”理论确定煤与瓦斯突出瓦斯压力临界值

通过实验分析得出了马家沟矿9—12、12煤层初始释放瓦斯膨胀能与瓦斯压力的线性关系，从而确定了马家沟矿深部水平9—12、12煤层煤与瓦斯突出瓦斯压力临界值，为深部水平煤与瓦斯突出预测提供了依据。     

Ba0.8La0.2MnAl11O19催化剂制备及其甲烷燃烧活性的研究

用共沉淀法制备了Ba0 8La0. 2MnAl11O19催化剂,并借助XRD、BET和SEM技术对其进行了表征,利用微型反应系统测定了催化剂的甲烷燃烧催化活性,研究了不同空速、烷氧比、甲烷体积分数下Ba0. 8La0. 2MnAl11O19的活性.结果表明,当空速为150 000h-1、烷氧比为1 /6、甲烷体积分数为3%时,甲烷燃烧的催化活性最好,完全转化温度为760℃.     

Influence of overpressure on coalbed methane reservoir in south Qinshui basin

In theory, from the high temperature and pressure during the coal generating gas to the present low temperature and pressure of coalbed methane reservoir, the accumulation of coalbed methane was from oversaturated to undersaturated. The gas content of the coalbed methane reservoir in the south Qinshui basin was 12-35.7 m3/t. According to the isotherm and measured gas content of No. 3 coal, the adsorbed gas content in some wells was highly saturated and oversaturated, which was hard to theoretically understand. In addition, there were no thermogenic and biogenic gases at the late stage in the south Qinshui basin. This article proposed that the overpressure was the main reason for the present high saturation of the coalbed methane reservoir. In early Cretaceous, the coalbed methane reservoir was characterized by overpressure and high saturation caused by gas generation from coal measure source rocks. In late Cretaceous, the coalbed methane reservoir was rapidly uplifted, and with the temperature and pressure decreasing, the pressure condition of adsorbed gas changed from overpressure to normal-under pressure, which resulted in the high saturation and gas content in the present coalbed methane reservoir.