活性炭纤维处理腐植酸废水

采用活性碳纤维处理腐植酸模拟废水,通过静态吸附和动态吸附的研究,测定吸附等温线和动态吸附曲线;研究不同温度、不同活性炭纤维、不同pH值和流速对处理效果的影响。     

南海高温高压含CO2气井管柱腐蚀适用性评价

目的 明确南海高温高压含CO2气井管柱材料腐蚀适用性,指导现场管柱材料选择.方法 采用高温高压釜腐蚀实验仪器对井筒高温高压环境条件下不同材料腐蚀速率进行实验分析,并采用扫描电镜及能谱分析仪对腐蚀实验后试样腐蚀形貌进行分析,评价不同井筒环境下管柱材料腐蚀适用性.结果 150℃条件下,材料腐蚀速率随分压的增加而增大,同时随...     

基于Landsat 8遥感数据的天津市地表温度反演

以Landsat 8遥感数据为数据源,进行天津市地表温度反演研究。首先采用单通道算法反演地表温度,并利用均值标准差法进行温度分级。然后建立不同温度等级面积比例的估算模型。再通过随机样点,从不同温度等级和土地覆盖类型2个角度,分别建立并比较不同类样点的地表温度与各指数的拟合模型。结果表明:次高温区域面积比例与人口密度、人均GDP都具有较高的决定系数;地表温度与NDVI、BAEM的二元线性回归决定系数高于地表温度与单一指数的决定系数;将样点分类后,低温点与MNDBI的决定系数高于其他温度等级样点,水域和植被样点与各种指数的决定系数高于其他地物类型样点。     

CO2和ABC干粉灭火剂扑灭火旋风火焰实验对比分析

为了分析2种灭火剂扑灭火旋风效果,采用实验室自制装置生成稳定的火旋风火焰,喷射CO₂或ABC干粉灭火剂,获取火焰温度场及光电信号数据。研究结果表明:在CO₂灭火剂或ABC干粉灭火剂作用下火旋风火焰温度场呈“下凹”型指数衰减;受灭火剂喷射位置影响,火焰根部、中部及顶端不同区域的灭火剂影响系数不同;基于火焰降温速率和光信号变化,相较于CO₂灭火剂,对火焰起抑制作用的ABC干粉灭火剂降温效率更高、扑灭效果更好。     

高温高压下煤孔隙结构的变化对瓦斯吸附特性的影响

为了研究高温高压条件下煤孔隙结构变化对瓦斯吸附特性的影响,选取九里山矿无烟煤,在压力为7 MPa、温度为40～130℃的条件下进行等温吸附实验和压汞实验。研究结果表明:煤样对甲烷的等温吸附曲线在该压力、温度条件下符合Ⅰ型吸附曲线特性,吸附规律符合Langmuir吸附模型;在压力7 MPa和温度130℃条件下,煤样的孔隙结构发生一定的变化,煤的比表面积增大、累计孔体积降低,可见孔及裂隙的数量比例增高,加强了煤样孔隙之间的连通度,导致原本吸附在煤样表面的甲烷分子大量解吸;在压力不变的情况下,随着温度的不断增高,煤的极限吸附量逐渐减小,其主要原因是样品孔隙结构的破坏和分子间作用力的变化。     

气象条件对静电除尘器低温腐蚀的影响分析

在已建成投产的静电除尘器当中,低温腐蚀是严重影响除尘器使用寿命的因素之一。以某烧结厂静电除尘器为研究对象,利用CFD软件,采用标准k-ε湍流模型对除尘器内部流场及温度场的分布进行数值模拟研究,得到静电除尘器内部流场和温度场分布特征,分析这些数据可知除尘器温度最低部位位于灰斗处,外界气温对壳体温度具有正相关的影响,在此基础之上有针对性地提出对静电除尘器壳体低温腐蚀的防治措施。     

振荡辐射下PMMA 热解与着火过程研究

采用正弦波变化振荡的辐射热流,对热厚PMMA(聚甲基丙烯酸甲酯)的热解和着火过程进行研究,同时采用数值模拟,对实验结果进行验证和补充。结果表明,表面温度和深度温度随着时间而增加,温度由于周期性的辐射而发生振荡,而振荡幅度随着深度的增加而衰减;表面温度与深度温度振荡存在时间延迟;着火时间随着热流振荡周期的增大而减小,主要由于平均热流密度随着周期增大而增大。     

单轴应力对煤自燃特性参数和导热系数的影响研究

为探究单轴应力作用下煤氧化和传热特性,利用自制荷载加压煤自燃特性参数测定装置对炉体内长焰煤煤样进行程序升温。结合程序升温过程中煤临界温度Tc和Tg,对其进行阶段划分:阶段1为30℃~Tc;阶段2为Tc~Tg。计算了不同单轴应力下2个阶段煤表观活化能和平均耗氧速率。根据能量守恒得出程序升温过程煤导热系数随温度的变化,进一步分析煤导热系数与单轴应力的关系。结果表明:阶段1单轴应力为4 MPa时为临界轴压,煤表观活化能最大,平均耗氧速率最小;阶段2煤表观活化能和平均耗氧速率随单轴应力增大均呈抛物线变化,单轴应力为2.7 MPa时为临界轴压,煤表观活化能最大,平均耗氧速率最小;阶段1和2煤导热系数随温度升高均先减小后增大,并且煤导热系数随单轴应力增大呈三次函数变化。     

17β-Estradiol mineralization under field and laboratory incubations

Mineralization studies of natural steroid hormones (e.g., 17β-estradiol, E2) are performed in environmental incubators, usually under a constant temperature such as 20°C. In this paper, we present a microcosm protocol that quantified the mineralization of E2 in soils under field temperatures. The nine agricultural soils tested had a wide range of soil organic carbon (1.1 to 5.2%) and clay (9 to 57%) contents. The calculated time over which half of the applied E2 was mineralized (E2-½) ranged from 299 to 910 d, and total E2 mineralization at 48 d (E2-TOT48) ranged from 4 to 13%. In subsequent laboratory incubations, the same soils were incubated under a constant temperature of 20°C, as well as under cyclic temperatures of 14.5°C (14 h) and 11.5°C (10h), which was within the temperature extremes observed in the field microcosms. E2-½ ranged from 157 to 686 d at 20°C and from 103 to 608 d at the cyclic temperatures, with the E2-TOT48 ranging from 6 to 21% at 20°C and from 7 to 30% under cyclic temperatures. Despite the overall 6.75°C lower mean temperatures under the cyclic versus constant temperatures, E2 mineralization was stimulated by the temperature cycles in three soils. Regardless of the incubation, the same loamy sand soil always showed larger E2 mineralization than the other eight soils and this loamy sand soil also had the smallest E2 sorption. Current modeling approaches do not take into consideration the effects of temperature fluctuations in the field because the input parameters used to describe degradation are derived from laboratory incubations at a constant temperature. Across the eight soils, E2-½ was on average 1.7 times larger and E2-TOT48 was on average 0.8 times smaller under field temperatures than under a constant 20°C. Hence, we conclude that incubations at 20°C give a reasonable representation of E2 mineralization occurring under field conditions to be expected in a typical Prairie summer season.     

Hot,Salty Water: A Confluence of Issues in Managing Stormwater Runoff for Urban Streams

Research increasingly highlights cause and effect relationships between urbanization and stream conditions are complex and highly variable across physical and biological regions. Research also demonstrates stormwater runoff is a key causal agent in altering stream conditions in urban settings. More specifically, thermal pollution and high salt levels are two consequences of urbanization and subsequent runoff. This study describes a demonstration model populated with data from a high gradient headwaters stream. The model was designed to explain surface water‐groundwater dynamics related to salinity and thermal pollution. Modeled scenarios show long‐term additive impacts from salt application and suggest reducing flow rates, as stormwater management practices are typically designed to do, have the potential to greatly reduce salt concentrations and simultaneously reduce thermal pollution. This demonstration model offers planners and managers reason to be confident that stormwater management efforts can have positive impacts.