活性炭C40/4吸附甲苯和丙酮吸附性能研究

为探讨活性炭吸附C40／4有机蒸汽的性能曲线规律，在不同温度288．15K，293．15K和298．15K下实验测试了活性炭C40／4吸附有机气体甲苯和丙酮的吸附性能，基于langmuir等温吸附理论，从吸附动态平衡的角度，理论分析了吸附性能曲线中参数与温度之间的关系，提出一个经验的langmuir等温吸附曲线模型，它能很好地描述不同温度下的有机蒸汽在活性炭上的吸附性能曲线，模型计算值与实验测试值之间的误差小于6％，为确定活性炭吸附有机蒸汽的吸附量提供了有效的计算模式，从而为有机蒸汽吸附过程的设计、预测和优化提供有益的支持。     

Behaviour of some pesticides in a nutrient-film and in a rock-wool system

Adsorption of ethoprophos, tetrachlorvinphos and etridiazole onto rock-wool was found to be much weaker than adsorption onto soils. The rates of transformation in water and in water plus rock-wool at 20°C were low. The concentration of etridiazole was measured in a nutrient-film system with recirculating nutrient solution. The decrease was rapid in the first few hours but was more gradual afterwards, to low values at 8 days after application. Etridiazole penetrated poorly into the lower part of a rock-wool system when the solution was trickled near the stem-base of the tomato plants.     

塿土不同粒级组分K+吸附研究

土各粒级K+吸附特征有很大区别.在一定平衡液浓度下,颗粒越细,土壤固相吸附量越大,不同粒级固相吸附量大小顺序是(＜0.1m)＞(＜1m)＞(1～2m)＞(2～5m),不同粒级土壤有效阳离子交换量也具有相同的变化规律.混合样中不同粒级组分对吸附的贡献可用吸附贡献率表示,土各粒级饱和吸附贡献率大小顺序为(＜1m)＞(1～2m)＞(＞5m)＞(2～5m),其中粘粒部分的饱和吸附贡献率为85%左右.在供试混合土样中＜1m粒级吸附贡献率随平衡液浓度增大呈幂函数形式增大,相反,1～2m、2～5m粒级吸附贡献率随平衡液浓度增大则呈幂函数形式减小.实验证明混合样中不同粒级K+吸附存在交互作用,吸附交互作用大小可用吸附交互作用系数表征,＜1m和1～2m之间存在吸附负交互作用,且随平衡液浓度增大而增强.＜1m和2～5m之间存在吸附正交互作用,且随平衡液浓度增大而减弱.论述了建立土壤多粒级组分吸附方程的必要性,提出了多粒级组分吸附方程q＝ρ(c)rifi(c)     

红壤对铝锰离子的吸附特征 Ⅲ.铝锰离子对的交换吸附

对具有水解性质的铝、锰离子对交换吸附研究的结果是 ,两种离子既表现了离子交换的一般化学行为 ,又有明显的非等当量交换和非电性吸附的特征 ;非等当量交换和非电性吸附受制于固相的表面性质、离子对的相对交换能力和离子的加入量 ;对非电性吸附的有关参数k、K、1/n、r和ΔF进行了表述 ;根据铝离子交换锰离子的ΔF ,从热力学论证了红壤对铝离子的吸附是自发和不可逆的并趋向稳态的自然过程     

Effect of low-molecular-weight organic acids on Cl- adsorption by variable charge soils

Low-molecular-weight (LMW) organic acids exist widely in soils and have been implicated in many soil processes.The objective of the present paper was to evaluate effect of two LMW organic acids, citric acid and oxalic acid, on Cl^- adsorption by three variable charge soils, a latosol, a lateritic red soil and a red soil, using a batch method. The results showed that the presence of citric acid and oxalic acid led to a decrease in Cl- adsorption with larger decreases for citric acid. Among the different soils Cl- adsorption in the lateritic red soil and the red soil was more affected by both the LMW organic acids than that in the latosol.     

螯合剂对沉积物中铬的去向的影响

A laboratory investigation on reaction between chelating agents and chromium was conducted to evaluate the effect of chelating agents on the adsorption and desorption of chromium in sediment. The amount of adsorbed chromium(Ⅵ) in sediment decreased slightly by 5%-10% because of addition of chelating agents. Chelating agents inhibited the removal of Cr(Ⅲ) by sediment from solutions and the inhibiting effect was in the order: citric acid > tartaric acid > EDTA, salicylic acid. No effect of chelating agents on desorption of chromium in sediment was observed.     

粘土土壤孔隙大小分布及其与土壤有机质的相关性

Soil pore size distribution(PSD) directly influences soil physical,chemical,and biological properties,and further knowledge of soil PSD is very helpful for understanding soil functions and processes.In this study,PSD of three clayey soils collected from the topsoil(0-20 cm) of Vertisols in Northern China was analyzed using the N_2 adsorption(NA) and mercury intrusion porosimetry(MIP) methods.The effect of soil organic matter(SOM) on the PSD of clayey soils was also evaluated.The differential curves of pore volume of clayey soils by the NA method exhibited that the pores with diameter 0.01 μm accounted for more than 50%in the pore size range of 0.001 to 0.1 μm.The differential pore curves of clayey soils by the MIP method exhibited three distinct peaks in pore size range of 60 to 100,0.3 to 0.4 and 0.009 to 0.012 μm,respectively.In the three clayey soils,the ultramicropores(5-0.1μm) were determined to be the main pore class(on average 35.5%),followed by macropores( 75 μm,31.4%),cryptopores(0.1-0.007μm,16.0%),micropores(30-5 μm,9.7%) and mesopores(75-30 μm,7.3%).The SOM greatly affected the pore structure and PSD of aggregates in clayey soils.In particular,SOM removal reduced the volume and porosity of 5-100 μm pores while increased those of 5 μm pores in the 5-2 and 2-0.25 mm aggregates of clayey soils.The increase in the volume and porosity of 5 μm pores may be attributed to the disaggregation and partial emptying of small pores caused by the destruction of SOM.     

热脱附-气相色谱质谱法测定挥发性有机化合物的研究

运用自动热脱附仪和气相色谱/质谱联用技术,通过对木制品中释放的多种挥发性有机物(VOCs)进行测试,得到较优的测试处理条件.研究发现,该方法的重现性和稳定性较好;较低的采样流速,可有效的降低苯在Tenax TA吸附管中的穿透行为.     

CMC粘接法制备柱状成型活性炭

以羧甲基纤维素钠(CMC)为粘接剂制备了柱状成型活性炭,研究了炭化温度、CMC添加量对产物吸附性能、孔结构及强度的影响。结果表明,随着炭化温度的升高,柱状成型活性炭的比表面积、亚甲基蓝吸附值和碘吸附值均呈现下降趋势;随着CMC添加量的增加,柱状成型活性炭的比表面积、总孔容、微孔容、平均孔径及亚甲基蓝吸附值、碘吸附值及对甲苯的吸附能力均逐渐降低,其强度逐渐增大。CMC粘接法制备柱状成型活性炭的最佳工艺为炭化温度200℃,CMC添加量10%,产物比表面积可达844.9 m2/g,亚甲基蓝吸附值和碘吸附值分别为189.2及968.2 mg/g,强度可达99.83%,甲苯的吸附率达65.5%。     

间歇灌溉对稻田毒死蜱迁移转化特征的影响

间歇灌溉作为丘陵区稻田常见的灌溉方式之一,其强烈的干湿交替过程会影响稻田中污染物的环境行为。在室内批量平衡吸附试验的基础上,通过农药野外喷施试验与动态观测,研究了间歇淹水和持续淹水条件下石灰性紫色土发育的稻田中毒死蜱的迁移转化特征。结果表明,土壤对毒死蜱的吸附能力远远强于其对毒死蜱主要降解产物3,5,6-三氯-2-吡啶醇(3,5,6-TCP)的吸附能力,毒死蜱的吸附容量常数范围为34~170,TCP的吸附容量常数范围为0.62~0.67,且对毒死蜱和TCP的吸附容量常数及分配系数均以耕作层土壤高于非耕作层土壤;施药后田面水中毒死蜱及TCP的浓度均随时间迅速下降,两者均可通过土壤大孔隙优先流快速迁移至50cm深处;间歇灌溉处理稻田土壤孔隙水中两者的浓度总体低于持续淹水处理;降雨和灌溉事件会导致两者由土壤固相迅速向水相发生短时间、高浓度释放与淋失。