钢渣对辽宁地区水稻土壤镉素吸收的影响

硅素肥料降低重金属毒性和减少重金属在植物体内积累的研究报道尚不多见。因此,开展这一领域的研究工作,将为合理应用硅素肥料修复、利用被重金属污染的土壤提供重要的理论依据。试验通过对辽宁不同地区水稻土施加钢渣,来研究钢渣对土壤吸附镉的影响。试验结果表明:施用钢渣能够增加大石桥、辽中、抚顺地区土壤对镉的吸附能力,而对盘锦、康平、苏家屯地区吸附能力影响不大;土壤对镉的等温吸附曲线,符合Langmuir等温吸附方程和Frendlich等温吸附方程,且加入钢渣前后,最大吸附量和吸附常数在不同程度上发生变化。     

沙柳活性炭对亚甲基蓝的吸附动力学和吸附等温线研究

为了提高沙柳的利用价值,获得一种成本低、性能好的活性炭,采用化学活化法,使用3种不同的活化剂制备沙柳活性炭,并研究其对亚甲基蓝溶液的吸附性能,探讨了活化温度、时间和p H值对亚甲基蓝吸附的影响,重点研究了不同活化剂制备沙柳活性炭的工艺条件以及沙柳活性炭吸附亚甲基蓝溶液的吸附等温线和吸附动力学曲线。研究结果表明:不同活化剂制备的活性炭其对亚甲基蓝的吸附量不同,其中氢氧化钾为活化剂时吸附量最大(519.63 mg/g),磷酸次之(347.13 mg/g),氯化锌最小(323.45 mg/g)。沙柳活性炭对亚甲基蓝溶液的吸附行为符合二级反应速率方程所描述的规律和Langmuir吸附等温式,p H值和温度的升高有利于吸附的进行。     

Phosphate adsorption by soils 1. Influence of time and ionic environment on phosphate adsorption

Abstract

The influence of reaction time and ionic environments, on phosphate adsorption were studied using one calcareous soil from India, and one calcareous and two latosols from Hawaii.

Phosphorus adsorption by soils has a initial rapid phase followed by a slow process. For plant nutrition studies, where emphasis is on P concentration of solutions from which plants derive P, isotherms should be constructed using data obtained after near‐equilibration has been attained. This condition does not obtain in a few hours and may require 6 days or more.

Calcium chloride as suspending electrolyte always gave lower phosphate solubility than when KC1 was used as electrolyte. Phosphate retention increased with increasing ionic strength. The necessity for obtaining clear supernatant solutions and the desirability for maintaining reasonable constant equilibrium conditions make 0.01 M CaCl₂ a reasonable choice for constructing P sorption isotherms, even though 0.01 M CaCl₂ is not representative of Ca concentrations in many soil solutions. Saturation extracts of soils investigated here were in the range 0.0002 to 0.005 M Ca.

Adsorption of calcium by highly weathered soils was high suggesting specific adsorption. Calcium adsorption was increased by phosphate additions to a Hydrandept.     

滤纸法测定非饱和土壤离子吸附等温线的初步研究

滤纸法对非饱和土壤溶液离子浓度的变化有较高的敏感性和较好的重现性 ,能够用于非饱和土壤离子吸附等温线的测定。滤纸法和乙醇浸提法、离心法有很好的一致性。滤纸法测定的非饱和土壤NH 4 、K 离子吸附等温线具有一般吸附等温线的共性 ,可用Freundlich方程描述 ,且达极显著相关水平。在土壤溶液浓度相同的情况下 ,液土比增大 ,离子固相吸附量增大 ,Freundlich方程的k值 ,n值增大 ,说明液土比增大有利于非饱和土壤离子吸附反应进行     

膨化干燥灰枣粉玻璃化转变及贮藏稳定性

为了综合水分活度及玻璃化转变理论构建状态图,获得灰枣粉的较佳贮藏条件,该文采用静态称量法和差示扫描量热法测定灰枣粉的吸附特性及玻璃化转变温度。结果表明,膨化干燥灰枣粉水分吸附的平衡干基含水率随水分活度的增加而增加,水分吸附等温线呈J型,描述灰枣粉水分吸附特性的适宜模型为GAB模型（R2=0.9968）;灰枣粉的玻璃化转变温度随含水率升高而降低,湿基含水率由0.064 g/g增加到0.175 g/g时,玻璃化转变温度由29.90℃降低到?35.02℃;灰枣粉干基含水率≤0.1223 g/g、贮藏温度≤?0.062°C时其稳定性较好,研究结果为灰枣粉加工、运输等过程中的贮藏条件提供理论参考。     

Comparison of the adsorption of maize root mucilage and polygalacturonic acid on montmorillonite homoionic to divalent lead and cadmium

Summary Root mucilage material (RM) was isolated from maize plants grown in the field, and its affinity to montmorillonite (M) homoionic to Pb²⁺ and Cd²⁺ was compared with that of a commercial polygalacturonic acid (PGA). Adsorption isotherms of the commercial and natural materials on the two clay systems were compared in unbuffered systems at pH 3 and pH 6. Adsorption of PGA occurred only at pH 3, and was higher on M-Pb than on M-Cd. In contrast, the adsorption of RM was higher on M-Cd than on M-Pb. Total amounts of RM adsorbed at pH 3 were about 3 times lower on M-Cd and 20 times lower on M-Pb than the respective amounts of PGA adsorbed at the same pH. Polygalacturonic acid had a high content of relatively well dissociated (pKa = 3.5) carboxylic groups, and adsorbed on the clay surface at pH values lower than its pKa. At pH 6, the dissociation of the acid groups favoured its solubility, and the metal cations were then probably displaced by ion exchange. The lower affinity of RM to the clay materials was related to its average molecular weight, which was lower than that of PGA, and to its water solubility, which was higher than that of PGA. The low pH dependence of the adsorption of RM was related to its lower carboxylic acidity and higher content in hydroxyl and amino groups.     

线性和非线性方法估计单宁酸共存下形成的无定形铝氧化物上菲的吸附等温线参数比较

采用批实验研究了菲在单宁酸干扰下形成的不同晶形铝氧化物上的吸附现象,并用不同的吸附等温线方程对吸附平衡数据进行了拟合,重点比较了线性和非线性回归方法估计吸附等温线参数的差异。结果表明:菲在各种晶形的铝氧化物上都有明显的吸附,但并不是完全随着单宁酸含量和结晶度的变化而规律性变化。吸附平衡数据以Langmuir、Redlich-Peterson和Dubinin-Radushkevich吸附等温方程,用不同的回归方法估计的等温线参数值均有显著性差异。线性回归得到的参数有不确定性,表明用线性回归来判断吸附等温线能否对吸附平衡数据进行最优拟合是不可靠的。相反,非线性回归能较好地确定菲在不同晶形铝氧化物上的最佳吸附等温线及相应参数。采用R2和χ2共同检验发现,菲在4种不同结晶度(单宁酸与铝的摩尔比(MR)=0,10-3,10-2,10-1)铝氧化物上的最佳吸附等温线方程并不尽相同,分别为Freundlich,Freundlich,Dubinin-Radushkevich和Freundlich,反映了各种晶形的铝氧化物的表面异质性。修正的Freundlich方程比较不同晶形铝氧化物对菲的相对吸附容量顺序为:MR=10-3MR=10-2MR=0MR=10-1。由此,认为菲在无定形铝氧化物上的吸附是熵驱动的结果。     

Approach to Determine Value of Variable Vapor Permeability of Autoclaved Aerated Concrete

The sorption isotherms and vapor permeability of autoclaved aerated concrete are obtained with the static gravimetric method and the cup method at 15℃, 25℃ and 35℃, respectively. The approaoh to determine value of variable permeability has been discussed. Meanwhile, it has been compared with the fixed value in Thermal Design Code for Civil Building (GB 50176-93). The results show that temperature dependence of the sorption isotherms and vapor permeability of autoclaved aerated concrete is small within test temperature range. Moreover, for adsorption process in medium or whole RH range, the average permeability obtained from our method is almost the same as that in the Code. This method can be extended to other porous building materials to obtain accurate permeability throughout whole RH range for both adsorption and desorption processes.     

Effects of Organic Matter-Rich Amendments on Selenium Mobility in Soils

Soil organic matter (SOM) plays an important role in the Se dynamics in soil. The potential effects of vermicompost and digestate as important sources of SOM on selenium (Se) mobility were assessed in this study. Three soils differing in their physicochemical parameters, fluvisol, chernozem, and luvisol, were chosen, and three types of vermicomposts based on various bio-waste materials as digestate (vermicompost 1), kitchen waste with woodchips (vermicompost 2), and garden bio-waste (vermicompost 3) were used due to their high organic matter content. Additionally, digestate samples alone were applied. To evaluate the potential effect of vermicompost application on sorption characteristics of soils, batch sorption experiments were performed. The results showed a predominant effect on Se species in the soils, where selenite sorbed more intensively compared to selenate, regardless of the soil and ameliorative material applied. In the control, the soil sorption ability of selenite tended to decrease in the order:fluvisol > luvisol > chernozem. However, these differences were not significant. Moreover, the effects of the ameliorative materials depended on both soil and amendment used. In fluvisol, all the amendment applications resulted in a decrease in distribution coefficient (K_d values) of Se, whereas in chernozem, this effect was observed only for the digestate-based vermicompost 1. Increasing K_d levels were reported in luvisol treated with digestate; the application of garden bio-waste-based vermicompost 3 tended to decrease the K_d values. Further studies are required on long-term effects of these amendments on Se mobility in soils and the role of individual organic matter fractions in this context.     

Characterization of clay and fine silt fractions of forest soils by standardized K/Ca sorption isotherms

For better comparison of selectivity characteristics of clay and fine silt fractions sorption isotherms standardized on the cation exchange capacity (CEC) are useful. Due to the effect of the CEC on the sorption isotherms, it is necessary to characterize the exchanging substance with regard to different ion selectivities with standardized potassium/calcium‐(K/Ca) sorption isotherms. This procedure helps to complete the knowledge about the mineralogical composition, which is obtained by X‐ray powder diffractometry. A Haplic Luvisol from boulder marl shows distinct differences in its K selectivity both between different particle size fractions and different horizons. This is partly due to the presence of smectites and vermiculites which are differently distributed within the particle size fractions. The increase of K selectivity with increasing particle diameter in the calcareous C horizon can be attributed to the marginal expansion of mica/illite by Ca²⁺ ions. The K selectivity of individual particle size fractions in different horizons of a Gleyic Cambisol from glacial sand shows major similarities. If pedogenic chlorite is formed, no changes in selectivity characteristics can be observed.