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51.
为解决农村稻秆的资源化利用问题,将稻秆用NaOH改性做吸附剂处理亚甲基蓝染料废水;考察pH值、吸附剂投加量、染料浓度和温度对染料吸附性能的影响;分析改性稻秆对亚甲基蓝染料的吸附动力学过程。研究结果表明,亚甲基蓝浓度为150mg/L,pH值为12、吸附剂投加量为4g/L时,改性稻秆对亚甲基蓝染料有很好的去除效果,染料的吸附率达到98.1%;改性稻秆对亚甲基蓝染料的吸附符合Freundlich等温模型,最大吸附量为52.910mg/g,升高温度能够增加吸附剂对亚甲基蓝染料的吸附效果;改性稻秆吸附亚甲基蓝是一个快速吸附过程,符合伪二级吸附动力学方程。 相似文献
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53.
竹炭对生物油模型组分的吸附特性试验 总被引:1,自引:0,他引:1
以竹子为前躯体热解制得竹炭,选取糠醛、乙酸、苯酚、葡萄糖为生物油模型化合物,研究竹炭对生物油模型组成各单组分的静态吸附特性及双、四组分混合下的竞争吸附行为。结果表明:竹炭对不同组分的吸附特性存在较大差异;单组分吸附24h,竹炭对糠醛的吸附量最大,乙酸次之,对葡萄糖的吸附量最小;吸附平衡时,竹炭对苯酚的吸附量将超过乙酸;糠醛-葡萄糖双组分竞争下,竹炭对糠醛显示出强烈的选择性吸附特征;4种组分竞争下,各组分吸附量相对单组分均有所下降,其中乙酸降幅最大,且乙酸等物质在吸附过程中出现浓度突变现象,这可能是因为吸附性能较好的糠醛将已经吸附的乙酸从竹炭上置换下来;在选用的所有试验工况下,竹炭对葡萄糖均表现出低的吸附态势。 相似文献
54.
针对餐饮废水含油量高,成分复杂等特点,采用格栅-沉淀-吸附工艺处理,经特质无纺布和改性纤维球过滤后(简称前处理)的餐饮废水,再利用核桃壳颗粒吸附,实验结果表明:不需要改变pH值前提下,投加核桃壳颗粒30g/L,吸附20min,振荡强度为120r/min,30℃时,对COD和含油量的去除率均达到69%以上。 相似文献
55.
对新疆盐碱地排碱渠渠水、水渠水、井水和塔里木河水水样进行了分析:其总盐量分别为12 915、11 352、9 980、1 421mg/L,根据水质评价标准当地水样主要有害盐分离子为Na+、Cl-,除塔里木河水外其他水样含盐量均严重超过了农业灌溉用水标准,未经任何处理的高盐农业废水对地下水体和公共水体都造成了一定的盐污染。对比分析各种水除盐方法,初步讨论采用价格低廉且具有良好选择吸附性能的钙基膨润土作为吸附剂对3号水样(水渠水:盐度为11 352mg/L)进行除盐。在固定温度50℃、搅拌速度为0.75m/s、吸附剂用量为5g(每100mL水样),搅拌1h后静置1d,总盐量降幅为23%,Na+浓度降幅为32%。此实验结果对高盐农业废水的再利用具有重要参考价值。 相似文献
56.
硫酸盐对锌和镉在可变电荷土壤上吸附的影响 总被引:8,自引:1,他引:8
SO4^2- and Zn^2 or Cd^2 were added to three variable charge soils in different sequences.In one sequence sulfate was added first ,and in the other,Zn^2 or Cd^2 first.The addition of sulfate to the system invariably caused an increase in adsorption of the heavy metal added,with the effect more remarkable whn the soil reacted with the sulfate prior to the metal.the shift in pH50 for both Zn and Cd adsorption was aslo comparatively larger in the first sequence of reactions .It was suggested that the increase in negative charge density and the resultant negative potential of the soil were the primary cause of the pronounced effect of sulfate on adsorption of Zn or Cd,and the formaiton of the ternary surface complex-S-SO4-M might also play a role in the effect. 相似文献
57.
谷物介电性质及其在含水量测量中的应用 总被引:3,自引:2,他引:3
对谷物介电性质的概念,测量方法、影响因子和预测模型进行了综述、介绍了利用介电性质测量谷物含水量的方法以及近期研究动向。 相似文献
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59.
As repeatedly reported, soil flooding improves the availability of P to rice. This is in contrast with an increased P sorption in paddy soils. The effects of soil flooding on the transformation of Fe oxides and the adsorption/desorption of P of two paddy soils of Zhejiang Province in Southeast‐China were studied in anaerobic incubation experiments (submerging with water in N2 atmosphere). Soil flooding significantly increased oxalate‐extractable Fe (Feox), mainly at the expense of dithionite‐soluble Fe (FeDCB), as well as oxalate‐extractable P (Pox), but decreased the ratio of Pox/Feox. Flooding largely increased both, P adsorption and the maximum P adsorption capacity. The majority of newly sorbed P in the soils was Pox, but also more newly retained P was found to be not extractable by oxalate. Flooding also changed the characteristics of P desorption in the soils. Due to a decrease of the saturation index of the P sorption capacity, P adsorbed by flooded soils was much less desorbable than that from non‐flooded soils. There are obviously significant differences in the nature of both, the Feox and Pox fractions under non‐flooded and flooded conditions. The degree of the changes in Feox, Pox, P adsorption and P desorption by flooding depended on the contents of amorphous and total Fe oxides in non‐flooded soils. Our results confirm that the adsorption and desorption behavior of P in paddy soils is largely controlled by the transformation of the Fe oxides. The reasons of the often‐reported improved P availability to rice induced by flooding, in spite of the unfavorable effect on P desorbability, are discussed. 相似文献
60.
Effects of NH4+ concentration, solution/soil ratio and temperature on NH4+ adsorption were studied in a Eum-Orthic Anthrosol. The slopes of the soil NH4+ adsorption isotherms and the fitted n, the coefficient for the adsorption intensity, and k, the coefficient related to adsorption capacity, of the Freundlich equation increased with increasing solution/soil ratio (SSR) and with decreasing temperature (T). For the range of experimental conditions, the value of ∂q/∂c, the rate of change of the amount of NH4+ adsorbed in the soil solid phase (q) with respect to the equilibrium concentration of NH4+ in soil solution (c), was 0.840, indicating that q increased with increasing c. From 2 to 45 ℃, ∂q/∂SSR, the rate of change of q with respect to SSR, decreased from 2.598 to 1.996, showing that q increased with increasing SSR, while its increasing rate decreased with temperature. From SSR 1:1 to 20:1, ∂q/∂T, the rate of change of q with respect to T, decreased from -0.095 to -0.361, indicating that q decreased with increasing temperature, and at the same time the negative effect of temperature became larger as SSR increased. Thus under the experimental conditions the order of importance in determining the amount of NH4+ adsorbed in the soil solid phase was ∂q/∂SSR > ∂q/∂c > |∂q/∂T|, indicating that the greatest effect on the amount of NH4+ adsorbed was with the solution/soil ratio; the equilibrium concentration of NH4+ had a lesser effect; and temperature had the least effect. 相似文献