天然纤维材料改性及其吸附抗生素的应用研究

以花生壳、木屑这些天然纤维材料制备吸附剂吸附废水中的四环素类抗生素,通过探讨改性剂种类、改性剂用量、改性时间等因素对吸附效果的影响,筛选出最佳吸附材料并优化改性方案。实验结果表明,两种吸附剂对抗生素废水均有较高的吸附效率,其中碱改性花生壳的吸附效果最好,最佳改性方案为1 mol·L-1 NaOH室温下改性5 h,对3种四环素类抗生素的去除率分别为土霉素67.27%、四环素79.08%、强力霉素87.40%。同时,利用傅立叶红外光谱（FTIR）和扫描电镜（SEM）对碱改性花生壳结构特性进行表征,推断碱改性花     

Retention and Uptake by Plants of Added Selenium in Peat Soils

In soil, adsorption of selenium (Se) onto mineral surfaces is accompanied by poorly known retention via organic matter. The effects of these components on the availability of Se were examined in two pot experiments. Spring wheat was grown with increasing amounts of selenate (SeO₄ ^2–) in one sand and three peat soils, and ryegrass with selenate and selenite (SeO₃ ^2–) in sphagnum peat manipulated by iron (Fe) hydroxide. Selenate persisted in soluble form, whereas selenite was fixed in the soil. In wheat, 5–50% of the selenate addition was recovered in the plant, the proportion increasing with increasing Se. In ryegrass, 30–40% of the added selenate but less than 2% of the selenite was found within the leaves. The Fe hydroxide enrichment enhanced the selenite uptake. Phosphate buffer desorbed a minor proportion of the added selenite, except in peat amply enriched with Fe hydroxide. The results suggest that the retention mechanism of selenite was changed due to the hydroxide amendment.     

Effect of Soil Properties on Boron Adsorption and Release in Arid and Semi-Arid Benchmark Soils

The adsorption isotherms indicated that the adsorption of boron (B) increased with its increasing concentration in the equilibrium solution. The Langmuir adsorption isotherm was curvilinear and it was significant when the curves were resolved into two linear parts. The maximum value of adsorption maxima (b1) was observed to be 7.968 mg B kg^?1 in Garhi baghi soil and the bonding energy (k) constant was maximum at 0.509 L mg^?1 in Jodhpur ramana soil. The Langmuir isotherm best explains the adsorption phenomenon at low concentrations of the adsorbent, which of course was different for different soils. There was significant correlation between b1 and clay (r = 0.905**), organic matter contents (r = 0.734*), and cation exchange capacity (CEC; r = 0.995**) of soils. A linear relationship was observed in all the soils at all concentration ranges between 0 and 100 mg B L^?1, indicating that boron adsorption data conform to the Freundlich equation. Soils that have a higher affinity for boron adsorption, like Garhi baghi, tended to desorb less amount of boron, that is, 43.54%, whereas Ballowal saunkhari desorbed 48.00%, Jodhpur ramana 48.42%, and Naura soil 58.88% of the adsorbed boron. Boron desorption by these soils is positively and significantly correlated with the sand content (r = 0.714**) and negatively with clay content (r = ?0.502*) and CEC (r = ?0.623**). The maximum value of 37.59 mg kg^?1 for desorption maxima (Dm) was observed in Garhi baghi soil and also a constant related to B mobility (Kd) was found to be maximum in Garhi baghi (0.222 L kg^?1) soil Note: *P<0.05; ^**P<0.01.     

Factors affecting the adsorption of micro‐amounts of tagged phosphorus by soils

Abstract

Adsorption of a small amount of P by soil from a solution, which delivers concentrations approximating the composition of soil solution systems, was measured for a heterogeneous group of 343 soils using ³²P‐labelled KH₂PO₄ solution. The method allowed accurate determination of small quantities of P and identified the P under consideration as that added from solution. Simple correlations and stepvise linear regression analyses indicated that soil pH, Ca, P, Al, Fe, organic matter and particle size significantly influenced the amount of P adsorbed by the soils.     

不同性质铁铝土对砷酸根吸附特性的比较研究

采用批平衡法研究了8种不同性质铁铝土对砷酸根的吸附特性,分别运用Langmuir单表面方程和Langmuir双表面方程对等温吸附数据进行拟合,以较优拟合方程求出土壤对砷的最大吸附量,并采用简单线性相关分析法探讨土壤性质对砷吸附能力的影响。结果显示,铁铝土对砷吸附强烈,吸附等温线均为非线性。双表面方程对吸附等温线的拟合效果优于单表面方程。采用双表面方程预测的吸附量和实测值的决定系数(0.935～0.978)大于采用单表面方程预测获得的决定系数(0.989～0.998)。土壤的砷吸附能力可采用高能表面和低能表面两种吸附位点进行解释。采集于云南昆明的砂页岩母质发育的红壤具有最强的砷吸附能力,根据Langmuir双表面方程计算的最大吸附量为3 498 mg kg-1。土壤的砷吸附能力受到土壤中游离氧化铁、全铝、全铁、黏粒和全磷含量的显著影响,最大吸附量与这几种土壤组成与性质因子呈显著正相关关系。     

天然膨润土的矿物特性及其磷吸附性能研究

比较了不同天然膨润土共7个样品对不同程度磷污染水体的吸附净化性能,通过等温吸附实验,探讨了膨润土对磷的吸附机制.结果发现,供试膨润土对水体磷均有一定的吸附净化潜力,但针对不同程度磷污染水体存在一定差异,且同一属型膨润土的吸附净化能力因矿物组成差异而不同.针对模拟V类水(P 0.4 mg/L)和劣V类水(P 1.0 mg/L),BN-2的吸附净化能力最强,BN-6的吸附净化能力较差,而其余膨润土对磷的吸附净化能力稍显差异.天然膨润土对磷的吸附等温曲线符合Freundlich方程,说明膨润土对磷的吸附可能属于不均匀介质的多分子层吸附.结果表明,在针对不同程度磷污染水体时,需根据膨润土的矿物特性,使各具特殊性质的不同天然膨润土矿样得到有效的应用.     

Molybdenum Determination in Mehlich‐1 and Mehlich‐3 Soil Test Extracts and Molybdenum Adsorption in Brazilian Soils

Abstract

The extractant Mehlich‐1 is routinely used in Brazil for determination of soil nutrients, whereas Mehlich‐3 has been suggested as a promising extractor for soil fertility evaluation. Both were used for extraction of molybdenum (Mo) in Brazilian soils with Mo dosage by the KI+H₂O₂ method. The Langmuir and Freundlich isotherms were used to study soil Mo adsorption. Mehlich‐1 extracted more Mo than Mehlich‐3 in soils with high contents of organic matter, clay, and iron (Fe) oxides. Mehlich‐3 and Mehlich‐1 extractions correlated positively and significantly with amorphous Fe oxides, crystalline Fe oxides, and organic matter. Molybdenum recovering rates correlated to crystalline Fe oxides and clay contents but not to organic matter, pH, and Mo adsorption capacity. Amorphous and crystalline Fe oxides, clay, and organic matter were responsible for most of the Mo adsorption. The Langmuir isotherm described better the Mo adsorption to soil amorphous Fe oxides and organic matter than the Freundlich isotherm.     

竹炭对生物油模型组分的吸附特性试验

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。     

低分子量有机配体对黏粒矿物吸附苏云金芽孢杆菌的影响

土壤是微生物的理想栖息地,土壤微生物群落组成复杂,数量巨大。1g土壤中可能栖息着上百亿个微生物,其中细菌可达1010个[1]。约80%～90%的土壤微生物寄居于土壤固相表面,如黏土矿物、金属氧化物或有机质表面[2]。细菌与矿物间的相互作用在土壤污染物转化与降解、团聚体形成[3]、矿物风化[4-6]及病原菌运移[7-8]等诸多过程起着关键作用。