不同改性黏土矿物吸附净化磷污染水体的性能比较

比较了酸、热及其复合改性对凹凸棒石黏土、膨润土和高岭土等3种黏土矿物吸附净化不同程度磷污染水体能力的影响。结果发现,2%浓度酸处理、300℃热活化及酸热复合改性均可以显著提高凹凸棒石黏土的磷吸附净化能力,且以复合改性效果最好,Ⅴ类和劣Ⅴ类水的磷去除率均比原土提高30%以上;酸、热改性均能显著提高膨润土的磷吸附净化能力,但综合不同程度磷污染水体来看,热活化略优于酸改性,但酸热复合改性没有呈现更佳的效果;热改性显著提高高岭土的磷吸附净化能力,而酸改性却不同程度地降低了高岭土的磷吸附净化能力,酸热复合改性的效果亦不如热单独改性。结果表明,在针对不同程度磷污染水体时需根据黏土矿物特性选用酸处理、热活化或酸热复合改性方法来提高污水的吸附净化效率。     

铁铝柱撑膨润土组成特征及其磷吸附性能研究

利用天然膨润土合成了铁柱撑膨润土（Fe1-Mt、Fe10-M）t、羟基铁膨润土（FeOx-M）t、羟基铝膨润土（AlOx-M）t和羟基铝铁膨润土复合体（AlFe-M）t,对其化学组成和矿物组成等特征进行分析,比较了5种不同铁铝柱撑膨润土对磷污染水体的吸附净化性能,并通过等温吸附试验探讨了柱撑膨润土对磷的吸附机制。结果发现,不同铁铝柱撑均可以增加天然膨润土的层间距,其中以羟基铝铁膨润土复合体的层间距增加最明显,与原土相比增加约为2倍。5种不同铁铝柱撑均能显著增强膨润土对磷污染水体的吸附净化能力,其中以FeOx-Mt的理论磷吸附容量最大,为12.03mg.g-1,其次为Fe10-Mt、AlFe-Mt和AlOx-Mt,吸附等温曲线同时符合Freundlich方程和Langmuir方程,均达显著水平。结果表明,除膨润土层间距外,不同铁铝柱撑膨润土的磷吸附能力主要与铁铝氧化物的含量及铁的存在形态相关。     

不同浓度酸改性对凹凸棒石黏土磷吸附性能的影响

比较分析了不同浓度酸改性凹凸棒石黏土对不同程度磷污染水体的吸附净化性能,并初步探讨了酸改性影响凹凸棒石黏土磷吸附性能的作用机制。结果发现,3%～30%酸改性可以不同程度地提高凹凸棒石黏土的磷吸附性能,其中以3%酸改性效果最好,在1%投加量下,其对Ⅴ类(P0·4mgL-1)和劣Ⅴ类(P1·0mgL-1)水磷的去除率分别达到95%和15%,而原土对磷污染水体基本无吸附净化能力。不同浓度酸改性不同程度地降低了凹凸棒石黏土的pH,可由原土的8·6降至3·86～3·35;3%～30%酸改性凹凸棒石黏土的zeta电位呈折线形变化,其中以3%酸改性凹凸棒石黏土的zeta电位最高,可达到-28·1mV。结果表明,酸改性可以通过改变凹凸棒石黏土的表面电荷和吸附活性位点等来提高它的磷吸附净化性能,且最适酸改性浓度不超过3%。     

改性高岭土对废水中磷的吸附性能及机理研究

采用盐酸和煅烧2种方法对苏州高岭土进行了改性,分析其对模拟含磷废水中磷的吸附效果,并初步探讨了其作用机制,继而进行了等温吸附和吸附动力学试验研究。结果显示,酸、热改性均不同程度地提高了高岭土对模拟废水中磷的吸附净化能力,尤以9%酸改性和500℃煅烧效果最为明显。在处理25 ml浓度为20 mg/L的模拟含磷废水中,高岭土投加量为2%(重量比)时,经9%酸改性高岭土对磷去除率达81.8%,较天然高岭土提高了44.6%。在处理50 ml浓度为20 mg/L的模拟含磷废水时,经500℃煅烧改性高岭土对磷的去除率高达99.5%,残留溶液中磷浓度仅为0.10 mg/L,达到我国相应排放标准。酸改性可通过改变高岭土的吸附活性点位来提高其对磷的吸附净化性能,而煅烧通过活化高岭石中的铝而提高其对磷的吸附净化性能。天然、9%酸改性及500℃煅烧高岭土磷吸附等温线均符合Freundilch和Langmuir方程,皆达极显著水平(P<0.01)。天然、9%酸改性及500℃煅烧高岭土对磷的动力学吸附特征一致,皆与准二级方程拟合最佳,达极显著水平(P<0.01)。500℃煅烧高岭土对磷的饱和吸附量最大,在净化含磷废水中具有良好的应用前景。     

荣成天鹅湖湿地沉积物对磷的吸附特征及影响因子分析

在荣成天鹅湖湿地的典型区域选取代表性样点,研究表层沉积物对水体中磷的吸附特征,并分析了环境因子、沉积物组成对磷吸附的影响.结果表明,当上覆水中磷浓度低于0.40 mg/L时,沉积物对磷的吸附量很低或呈负吸附状态;在高磷浓度条件下,等温吸附曲线可用改进的Langmuir模型来很好地拟合.本研究条件下湿地沉积物对磷的吸附容量(Q_(max))变幅为181.8～1 000.0 mg/kg.临界磷平衡浓度(EPC_0)变化在0.043～0.479 mg/L之间.沉积物对磷的最大吸附量与其本身的理化性质关系密切,主要影响因素为粘粒含量和粘土矿物种类,氧化铁铝和有机质含量起次要作用.环境因子对磷吸附的影响作用明显,各因子的影响顺序为:扰动>温度、盐度>pH.不同区域相比,湿地北部沉积物的吸附能力远高于南部砂质土.且后者的吸附特性更易受到环境因子的影响.     

天鹅湖沉积物对磷的吸附动力学及等温吸附特征

以荣成天鹅湖这一天然泻湖为研究对象,研究了6个样点沉积物对磷的吸附动力学曲线和等温吸附方程,并分析了沉积物理化性质与磷吸附参数间的关系.结果表明,天鹅湖不同区域沉积物对磷的吸附动力学均符合二级动力学方程,吸附反应主要在前10h内完成,且0～2h内反应迅速.根据Langmuir模型,6个样点沉积物对磷的理论吸附容量(Qmax)的范围为294.12～1 111.11 mg/kg,其中湖区北部和中部沉积物的吸附能力高于南部.沉积物对水体中磷的吸附解吸平衡浓度(EPC0)的变幅为0.002 ～ 0.033 mg/L,其与沉积物本底吸附态磷(NAP)呈较弱的正相关关系.本研究条件下,大部分样点的EPC0小于上覆水中磷的浓度,其中湖区西北部和东南部沉积物中磷具有向上覆水体释放的趋势.沉积物的NAP与总氮、有机质、活性铝和黏粒间均呈显著正相关,Qmax与铁铝结合态磷、有机质、活性铝和粉粒间呈显著的正相关关系.活性铝、有机质和粒度是影响沉积物磷吸附的主要因素.     

四种典型重金属污染对土壤吸附磷的影响

以空白土壤和人工制备的不同浓度铜、砷、镉和铅污染土壤为对象,研究了在不同pH值、温度和柠檬酸浓度条件下重金属污染对土壤吸附磷的影响,并对其进行了相关过程的等温和吸附动力学的机理分析。研究结果表明,空白土壤和As污染土壤吸附磷的等温吸附过程符合Temkin方程,Cu、Pb、Cd污染土壤吸附磷的等温吸附过程符合Freundlich方程,空白土壤和重金属污染土壤吸附磷的动力学过程均符合Elovich方程;重金属污染对土壤吸附磷有一定的抑制作用,抑制程度与污染物浓度呈现显著的正相关,且随外在环境因子的改变而不同。当重金属元素铜、铅、砷、镉的含量分别为200、80、25、0.8 mg kg^-1时:pH值为5时,重金属对土壤吸附磷抑制作用最小,土壤吸附磷量分别降低了30.18%、13.54%、30.74%、37.23%,其抑制作用程度为:Cd> As> Cu> Pb;土壤吸附磷量与温度呈现显著的正相关,温度变化为25~45℃时,土壤对磷的吸附量分别增大了17.14%~28.83%、6.72%~16.05%、8.68%~9.13%、10.30%~23.45%,同一条件下重金属对土壤吸附磷抑制作用程度为Cu> Cd> As> Pb;重金属污染土壤吸附磷量与柠檬酸浓度成负相关,柠檬酸浓度为50 mg L^-1时,土壤吸附磷量分别降低了19.87%、21.94%、23.18%、24.84%,相同柠檬酸浓度下其抑制作用程度为Cd> As> Pb> Cu。     

6种水生植物及其组合对模拟污水中磷的净化效果

[目的]针对河流湖泊水体污染严重现状,选择6种水生植物进行水质净化试验,为污染水体的水生植物治理提供选择依据。[方法]选择6种具观赏效果的水生植物菖蒲、美人蕉、大薸、凤眼莲、金鱼藻、穗花狐尾藻,采用静态水培的方法,研究6种水生植物及其组合对不同浓度模拟污水中总磷净化效果。[结果]单一水生植物试验中,凤眼莲在高(2 mg/L)、中浓度(0.5 mg/L)磷水体中总磷去除效果最好,去除率分别为95.9%,93.4%。金鱼藻在低浓度磷(0.1 mg/L)水体中总磷去除效果最好,去除率为91.1%。组合水生植物试验中,高浓度磷水体中金鱼藻+菖蒲+凤眼莲的水生植物组合对水体中总磷去除效果最好,去除率为96%。中浓度磷水体中穗花狐尾藻+菖蒲+凤眼莲水生植物组合总磷去除效果最好,去除率为98.8%。低浓度磷水体中穗花狐尾藻+菖蒲+大薸水生植物组合总磷去除效果最好,去除率为94.3%。[结论]选择的6种水生植物对总磷均有一定的去除效果,对水生植物的种植数量、面积、时间以及组合方式进行优化配置,可用于污染水体水质净化。     

水铁矿对磷的吸附及胶体态磷迁移能力预测

土壤中流失的磷进入水体容易引起富营养化污染。目前对于铁矿物胶体结合态磷在土壤孔隙介质中的稳定性和迁移能力的认识还存在不足。本研究采用吸附试验,考察水铁矿对磷的吸附特征以及pH、离子强度和胡敏酸对磷在液相、水铁矿胶体和水铁矿固体上分布的影响;通过DLVO理论,预测水铁矿胶体结合态磷的稳定性和迁移能力。结果表明,假二级动力学模型(R~2=0.964)更适合用于描述磷在水铁矿上的吸附过程,磷在水铁矿上的吸附受液膜扩散、内部扩散和化学吸附等过程控制。Freundlich模型(R2=0.970)对等温吸附的拟合效果好,说明水铁矿对磷的吸附为多层吸附过程。从Langmuir模型参数可知,水铁矿对磷的最大理论吸附量为22.55mg·g~(-1)。水铁矿对磷的吸附能力随pH的升高而降低,随离子强度的升高而升高。然而,低离子强度和高pH有利于反应体系中水铁矿胶体的释放。无论胡敏酸是否存在,在碱性且离子强度不高(1～10mmol·L~(-1))的条件下,有约5%～20%的磷会与水铁矿胶体结合,且这些磷-水铁矿胶体之间的静电斥力较大。根据DLVO理论计算可知,这些带负电荷的胶体之间稳定性较好,在土壤中有一定迁移能力。在实际农业活动中,磷肥的过量施用可能会使大量的磷酸根离子吸附在铁矿物上,促进土壤孔隙水中形成稳定的、带负电的铁矿物胶体,这种磷-铁矿物复合胶体的迁移很可能成为磷迁移的另一种形式。本研究结果可为胶体促进下磷淋失风险评估提供理论和数据支撑。     

离子强度和磷酸盐对铁铝矿物及土壤吸附As（V）的影响

选用针铁矿、赤铁矿、水铁矿、水铝矿4种铁铝矿物以及性质差异较大的黑土、紫色土和红壤3种土壤,研究离子强度和磷酸盐对其吸附As（V）的影响。结果表明,在0．01、0．1、1mol·L^-13种离子强度下,矿物和土壤对As（V）的吸附量无明显差异或随离子强度增大而增大,其对砷的吸附以专性吸附为主。磷酸盐对矿物和土壤吸附砷的影响与其添加顺序及摩尔浓度比有关。水铝矿和水铁矿在这3种添加顺序下的砷吸附量无明显差异,仅在P／As摩尔比较大时表现出下降趋势;而在针铁矿和赤铁矿两种矿物上,先添加砷时的砷吸附量高于先添加磷时或两者同时添加时,且砷吸附量随WAs摩尔比的增加而逐渐下降。在黑土、紫色土和红壤上,先添加砷比先添加磷或两者同时添加时的砷吸附量均要高,尤其是在紫色土上。随P／As摩尔比升高,土壤对砷的吸附量表现出下降趋势。     

Effects of Municipal Sewage Sludge Application on Soil and Purple Moor-grass (Molinia caerulea) Contamination by Metals in a Maritime Pine Forest

Granular bentonite has been assessed regarding its capacity to remove Hg(II), Cd(II) and Pb(II) from aqueous solutions. Sorption capacities, kinetics and the dependence of the sorption process on pH were determined. Fractional power, pseudo-first-order, pseudo-second-order and intra-particle diffusion equations were used to model the kinetics of metal adsorption. The pseudo-second-order model showed the best fit to experimental data. Different two-parameter sorption isotherm models (Langmuir, Freundlich, Temkin and Dubinin?CRadushkevich) were used to fit the equilibrium data. Freundlich's isotherm model gave the best fit to experimental data. The selectivity of granular bentonite towards these metals is Pb(II)?>?Cd(II)?>?Hg(II). The adsorption capacities of granular bentonite towards the metals expressed in milligramme metal per gramme granular bentonite are 19.45, 13.05 and 1.7 for Pb(II), Cd(II) and Hg(II), respectively (for an initial concentration of 100 mg metal/L).     

Effect of Continuous Vegetable Cultivation on PhosphorusLevels of Fluvo-Aquic Soils

oil P status, inorganic P fractions, and P sorption properties were studied using sandy fluvo-aquic horticultural soils,which are high in organic matter content for vegetable production in comparison with a soil used for grain crop productionin Zhengzhou, Henan Province, China. P fractions, Olsen-P, and OM were determined at different depths in the soilprofile and sorption isotherm experiments were performed. Most P in excess of plant requirements accumulated in thetopsoil and decreased with soil depth. Total P, inorganic P, and OM concentrations increased with continued horticulturaluse.Olsen-P concentrations in the 0-20 cm depth of horticultural soils were 9 to 25 times higher than those of the graincrop soil. A linear transformation of the Langmuir equation showed that the P adsorption maximum (491.3 mg P kg^-1)and the maximum phosphate buffering capacity (162.1 L kg^-1) for 80-100 cm were greater in the grain crop soil than thehorticultural soils. Thus, the most immediate concern with excess P were in areas where heavy P fertilizer was used forvegetable crops and where soil P sorption capacities were low due to sandy soils and high organic matter content.     

Reduction of ochratoxin a levels in red wine by bentonite, modified bentonites, and chitosan

Adsorption method may play an important role to remove ochratoxin A (OTA) from wine by bentonite (B), nonylammonium bentonite (NB), dodecylammonium bentonite (DB), KSF-montmorillonite (KSF), and chitosan bead (CB). The optimum conditions of OTA adsorption from synthetic solutions were revealed at room temperature and pH 3.5. The adsorption equilibria of B and NB were almost established within 120 and 240 min, respectively. DB, KSF, and CB had about 90 min of equilibration time. The adsorption efficiency carried out in the synthetic OTA solution did not change remarkably when the amounts of adsorbents were 25 mg for bentonite, DB, and KSF and 100 mg for NB and CB. Furthermore, 25 mg of adsorbents was used at all adsorption studies in synthetic solution. The adsorption isotherm was fitted with mostly a Freundlich equation with respect to the correlation coefficients. The adsorption data were evaluated using Langmuir and Freundlich equations having Kf values ranging from 0.011 to 9.5 with respect to correlation coefficients (R2 = 0.900-0.977). DB and KSF have the highest adsorption capacity for OTA in synthetic solutions. In wine, the removal of OTA was succeeded at a percentage of 60-100 by KSF and CB. Furthermore, the highest adsorption capacity of OTA for red wine was obtained by using 250 mg of KSF, which caused less damage to the nature of wine and also low adsorption of polyphenols and anthcyans.     

Adsorption and desorption properties of macroporous resins for anthocyanins from the calyx extract of roselle (Hibiscus sabdariffa L.)

Adsorption of roselle anthocynins, a natural pigment, onto various macroporous resins was optimized to develop a simple and efficient process for industrial separation and purification of roselle anthocyanins. Nine different macroporous resins (AB-8, X-5, HPD-100, SP-207, XAD-4, LS-305A, DM-21, LS-610B, and LS-305) were evaluated for the adsorption properties of the anthocyanins extracted from the calyx extract of Hibiscus sabdariffa L. The influences of phase contact time, solution pH, initial anthocyanin concentration, and ethanol concentration with different citric acid amounts were studied by the static adsorption/desorption method. The adsorption isotherm data were fitted well to the Langmuir isotherm, and according to this model, LS-610B and LS-305 exhibited the highest monolayer sorption capacities of 31.95 and 38.16 mg/g, respectively. The kinetic data were modeled using pseudo-first-order, pseudo-second-order, and intraparticle diffusion equations. The experimental data were well described by the pseudo-second-order kinetic model. Continuous column adsorption-regeneration cycles indicated negligible capacity loss of LS-305 during operation. The overall yield of pigment product was 49.6 mg/g dried calyces. The content of roselle anthocynins in the pigment product was 4.85%.     

连续种植蔬菜对潮土磷素水平的影响

Soil P status, inorganic P fractions, and P sorption properties were studied using sandy fluvo-aquic horticultural soils, which are high in organic matter content for vegetable production in comparison with a soil used for grain crop production in Zhengzhou, Henan Province, China. P fractions, Olsen-P, and OM were determined at different depths in the soil profile and sorption isotherm experiments were performed. Most P in excess of plant requirements accumulated in the topsoil and decreased with soil depth. Total P, inorganic P, and OM concentrations increased with continued horticultural use. Olsen-P concentrations in the 0-20 cm depth of horticultural soils were 9 to 25 times higher than those of the grain crop soil. A linear transformation of the Langmuir equation showed that the P adsorption maximum (491.3 mg P kg^-1) and the maximum phosphate buffering capacity (162.1 L kg^-1) for 80-100 cm were greater in the grain crop soil than the horticultural soils. Thus, the most immediate concern with excess P were in areas where heavy P fertilizer was used for vegetable crops and where soil P sorption capacities were low due to sandy soils and high organic matter content.