漓江流域δD和δ18O对蒸发的指示作用

以漓江流域为例查明不同水体之间氢氧稳定同位素组成特征,并探讨氢氧稳定同位素对漓江流域的蒸发过程指示作用.结果表明：流域内不同水体之间,氢氧稳定同位素表现出不同的组成特征,地表水和地下水,在丰水期δD值和δ¹⁸O值要比枯水期更容易富集,地下水的δD值和δ¹⁸O值分布范围较地表水小;随着水温的升高,δ¹⁸O的变化趋势比d-excess明显.从漓江上游到下游高程逐渐下降,河水线的斜率和截距也在逐渐减小,其中漓江下游河水线的斜率和截距要低于当地大气降水线,表明下游受到蒸发作用较强烈;地下河水线、地表河水线在一定程度上偏离当地大气降水线,但偏离程度较小,表明三者之间有很好的水力联系.受温度和湿度的共同影响,漓江干流丰水期河水的蒸发量占最初水体总量的0.7%~9.1%,枯水期河水的蒸发量占最初水体总量的2.6%~9.7%,丰水期的蒸发比例低于枯水期,从上游到下游蒸发比例在逐渐上升.研究区蒸发量估算值为959.40mm,与多年实测值少43.11mm,相对误差4.70%.氢氧稳定同位素对研究区降水、地表水、地下水之间的转换规律具有重要的实际意义,在今后的漓江流域水文研究中有着更加广阔的空间.     

飞机喷洒农药的损失分析

通过田间试验，对装配ＧＰ－８１扁扇型喷头的运５飞机在水稻和棉花上喷洒农药中的药液损失进行了分析，同时讨论了２，４－Ｄ丁酯对敏感作物的影响。结果表明，一元三次方程Ｙ＝ｂ０＋ｂ１ｘ２＋ｂ２ｘ＾２＋ｂ３ｘ＾３能很好地描述药液飘移与下风距离的关系，方程中的参数具有明确的实验意义；２，４－Ｄ丁酰对７００ｍ下风距离内的向日葵类高敏感植物有明显药害，对３５０ｍ范围内的大豆等中等敏感植物也有药害；药液由于飘移和蒸     

QUALITY OF HYDROMETEOROLOGICAL DATA IN COLD REGIONS1

ABSTRACT: Many users of hydrometeorological records are not aware of the number of inconsistencies and biases that occur in hydrometeorological records. Examples are presented illustrating how the exposures of sites for measurement of precipitation, wind, snow on the ground, and evaporation determine to a large extent how useful the records are for estimating areal conditions. For areas where precipitation in the form of snow produces a significant portion of the runoff, a smaller number of quality records may be more valuable for modeling than a much larger number of records of lower quality. Information is presented to show that the overall value of an operational hydrometeorological network is dependent upon how consistent and representative of average conditions the collected records are, especially for mountainous areas in cold regions.     

利用单片机实现对云台的转动控制

以单片机为核心，将单片机的串口通过RS-485与云台相连，采用RS-485总线标准，通过PELCO—P协议，在C51环境中编制程序，实现了对(多台)云台的方位转动控制。     

硅藻土负载型非均相芬顿催化剂制备及其降解苯酚的实验研究

以硅藻土为载体,采用直接蒸发法负载铁的氧化物,制备了一种新型负载型非均相芬顿催化剂,通过SEM、EDS和XRD等对催化剂进行了表征,并以苯酚去除率考察了催化剂性能。结果表明:铁氧化物可成功负载于硅藻土上;催化剂制备时最优铁离子浓度和固液质量比分别为0.5 mol/L和1∶10;催化剂重复使用性高,耐酸碱性良好,对苯酚的去除率可达99%以上。催化剂利用了硅藻土优异的物化性质,对难降解有机废水具有良好的应用前景。     

汽油在西北黄土上吸附特性的研究

通过动力学和热力学吸附实验,研究了汽油在西北地区黄土上的吸附行为,同时研究了提取的天然腐植酸对汽油在黄土上吸附行为的影响.结果表明,汽油在黄土上的吸附在6h内达到平衡.无论是否加入腐植酸,汽油在黄土上的吸附动力学过程均符合Elovich方程,其热力学吸附符合Freundlich方程.腐植酸的存在使汽油在黄土上的吸附能力减小.反应温度从25℃升高到45 C,汽油在土壤上的饱和吸附量从6.300mg·g-1减小到1.365 mg·g-1,表明汽油在黄土上的吸附属于放热反应.溶液pH和土壤粒径的增大,均不利于汽油在黄土上的吸附,溶液pH和土壤粒径越大,其在黄土上的吸附量越小.另外,在室温下对吸附了汽油的土壤样品和纯汽油挥发行为的研究表明,吸附了汽油的土壤样品的汽油挥发比纯汽油慢,其挥发率与时间成对数关系.     

Identification of key factors governing chemistry in groundwater near the water course recharged by reclaimed water at Miyun County, Northern China

Reclaimed water was successfully used to recover the dry Chaobai River in Northern China, but groundwater may be polluted. To ensure groundwater protection, it is therefore critical to identify the governing factors of groundwater chemistry. Samples of reclaimed water, river and groundwater were collected monthly at Chaobai River from January to September in 2010. Fifteen water parameters were analyzed. Two kinds of reclaimed water were different in type (Na-Ca-Mg-Cl-HCO3 or Na-Ca-Cl-HCO3 ) and concentration of nitrogen. The ionic concentration and type in river were similar to reclaimed water. Some shallow wells near the river bed had the same type (Na-Ca-Mg-Cl-HCO3 ) and high concentration as reclaimed water, but others were consistent with the deep wells (Ca-Mg-HCO3 ). Using cluster analysis, the 9 months were divided into two periods (dry and wet seasons), and all samples were grouped into several spatial clusters, indicating different controlling mechanisms. Principal component analysis and conventional ionic plots showed that calcium, magnesium and bicarbonate were controlled by water-rock interaction in all deep and some shallow wells. This included the dissolution of calcite and carbonate weathering. Sodium, potassium, chloride and sulfate in river and some shallow wells recharged by river were governed by evaporation crystallization and mixing of reclaimed water. But groundwater chemistry was not controlled by precipitation. During the infiltration of reclaimed water, cation exchange took place between (sodium, potassium) and (calcium, magnesium). Nitrification and denitrification both happened in most shallow groundwater, but only denitrification in deep groundwater.     

含汞原料中汞挥发速率的测试方法研究

以PVC行业废汞触媒、糊式锌锰电池浆液、含汞锌膏为原料,采用动力通量箱法测试其挥发速率,研究了最佳试验操作条件。结果表明:通量箱气体流速在0.5 L/min以下,采用两级大型气泡吸收管吸收挥发汞时效率可达99%以上,增加1次空白测量可测得通量箱壁汞吸附量。     

铬盐废水蒸发系统腐蚀突变与缓蚀工况研究

针对铬盐废水蒸发系统运行过程中的腐蚀问题,采用失重法、pH值检测、扫描电镜(SEM、EDS)和XRD等手段,模拟研究了温度、Cr3+质量浓度对20#碳钢腐蚀速率、腐蚀产物的影响,并从废水pH值和形貌分析角度探索腐蚀速率发生突变的原因.研究表明:废水Cr3+质量浓度在150～180 mg/L范围,碳钢腐蚀速率发生突增,废...     

Effect of soil moisture dynamics on dense nonaqueous phase liquid (DNAPL) spill zone architecture in heterogeneous porous media

The amount, location, and form of NAPL in contaminated vadose zones are controlled by the spatial distribution of water saturation and soil permeability, the NAPL spill scenario, water infiltration events, and vapor transport. To evaluate the effects of these processes, we used the three-phase flow simulator STOMP, which includes a new permeability-liquid saturation-capillary pressure (k-S-P) constitutive model. This new constitutive model considers three NAPL forms: free, residual, and trapped. A 2-D vertical cross-section with five stratigraphic layers was assumed, and simulations were performed for seven cases. The conceptual model of the soil heterogeneity was based upon the stratigraphy at the Hanford carbon tetrachloride (CT) spill site. Some cases considered co-disposal of NAPL with large volumes of wastewater, as also occurred at the Hanford CT site. In these cases, the form and location of NAPL were most strongly influenced by high water discharge rates and NAPL evaporation to the atmosphere. In order to investigate the impact of heterogeneity, the hydraulic conductivity within the lower permeability layer was modeled as a realization of a random field having three different classes. For six extreme cases of 100 realizations, the CT mass that reached the water table varied by a factor of two, and was primarily controlled by the degree of lateral connectivity of the low conductivity class within the lowest permeability layer. The grid size at the top boundary had a dramatic impact on NAPL diffusive flux just after the spill event when the NAPL was present near the ground surface. NAPL evaporation with a fine grid spacing at the top boundary decreased CT mass that reached the water table by 74%, compared to the case with a coarse grid spacing, while barometric pumping had a marginal effect for the case of a continuous NAPL spill scenario considered in this work. For low water infiltration rate scenarios, the distribution of water content prior to a NAPL spill event decreased CT mass that reached the water table by 98% and had a significant impact on the formation of trapped NAPL. For all cases simulated, use of the new constitutive model that allows the formation of residual NAPL increased the amount of NAPL retained in the vadose zone. Density-driven advective gas flow from the ground surface controlled vapor migration in strongly anisotropic layers, causing NAPL mass flux to the lower layer to be reduced. These simulations indicate that consideration of the formation of residual and trapped NAPLs and dynamic boundary conditions (e.g., areas, rates, and periods of different NAPL and water discharge and fluctuations of atmospheric pressure) in the context of full three-phase flow are needed, especially for NAPL spill events at the ground surface. In addition, NAPL evaporation, density-driven gas advection, and NAPL vertical movement enhanced by water flow must be considered in order to predict NAPL distribution and migration in the vadose zone.