水稻土团聚体中Cu~(2+)的解吸动力学特征

用磁力搅拌法和平衡吸附法研究了水稻土的原土和团聚体颗粒吸附态Cu2+的解吸动力学特征.结果表明,原土和团聚体颗粒Cu2+的解吸率大小顺序为粗粉砂级粉砂级原土砂粒级粘粒级,与其有机质、游离氧化铁、氧化铝含量大小顺序相反.Cu2+解吸过程可分为快、慢两个解吸阶段,快解吸阶段属于非专性吸附态Cu2+的解吸,慢解吸阶段属于专性吸附松结合态Cu2+的解吸.用一级动力学方程、E lovich方程和双常数方程模拟Cu2+的解吸过程,相关性均达显著水平.磨细后的原土Cu2+的解吸速率和解吸进度均大于4个粒组团聚体颗粒.Cu2+的解吸速率和解吸量与土壤表面Cu2+的吸附形态有关.     

三峡水库消落区土壤汞吸附解吸动力学特征

对三峡水库消落区5种土壤进行了汞的吸附-解吸试验,用不同的等温吸附方程和化学反应动力学方程进行了模拟比较,结果显示,不同土壤对汞的吸附解吸动力学规律相类似,吸附速率和解吸速率均与土壤pH值呈显著(r=0.933,p＜0.05)和极显著相关性(r=0.962,p＜0.01),但吸附量和解吸量各不相同,其中,紫色潮土对汞的吸附量最大,酸性紫色土最小;灰棕潮土对汞的解吸量最大,黄壤最小,其它类型土壤介于它们之间.     

珠江悬浮物对0号柴油的吸附与解吸实验

通过室内实验,分析了悬浮物对0号柴油乳化油吸附、解吸的基本规律,并对泥沙浓度和温度因素影响进行了研究。实验结果表明,悬浮物对0号柴油的吸附和解吸过程符合一级动力学过程;悬浮物的平衡吸附量随着液相平衡浓度的升高而趋于平缓,Langmuir方程和Freundlich方程都能较好的反映珠江广州段泥沙的吸附规律;固相平衡吸附浓度随着悬浮物浓度的升高而降低,而液相解吸平衡浓度则随着悬浮物浓度的升高而增加;此外,温度的升高不利于柴油吸附过程而更有利于解吸过程。     

菜园土壤铜吸附--解吸特性的研究

研究了菜园土壤铜的吸附—解吸特性。结果表明 ,3种菜园土壤吸附 Cu2 的量均随平衡液中Cu2 浓度的增加而增大 ,可用 L angmuir方程和 Freundlich方程来描述。由 Langmuir方程求得的菜园土壤对 Cu2 的最大吸附量和最大缓冲容量的大小顺序为 :黄松土 >江涂土 >粉泥土 ,菜园土壤对 Cu2 的解吸量和解吸率均随其吸附量的增加而增加 ,吸附量与解吸量之间呈显著或极显著线性正相关。     

草炭土及其有机质组分对PCB138吸附动力学和热力学研究

选取六氯联苯PCB138为目标污染物,有机质含量较高的草炭土为供试土壤,提取草炭土中的胡敏酸和胡敏素,研究PCB138在草炭土原土壤、胡敏酸和胡敏素中的吸附动力学和热力学。实验结果表明,PCB138在草炭土原土壤、胡敏酸和胡敏素中的吸附是一个快速吸附过程,240 min后吸附达到动态平衡,吸附速率常数分别为0.014、0.011、0.005,吸附速率由快到慢依次为原土壤胡敏酸胡敏素。准一级、准二级、Elovich和Weber-Morris动力学模型分析结果显示,准二级动力学模型能更好地描述其吸附过程,可决系数r2在0.988—0.994间。在实验条件下,随着PCB138在土壤中浓度增大,土壤各组分对其吸附量也随之增大。温度由25℃升高到45℃时,土壤各组分对PCB138的吸附量由1.40—17.7μg·g~(-1)增长到1.56—17.9μg·g~(-1),即随着温度的升高吸附量略有增大。热力学吸附过程采用Freundlich、Langmuir和Temkin等温吸附模型进行拟合,拟合结果显示,Freundlich等温吸附模型拟合效果更好。在吸附时间为240 min的实验条件下,计算得到的有机碳均一化分配系数Koc值表明PCB138在胡敏酸中吸附能力最强。由吉布斯方程得到的3个热力学参数:吸附自由能(ΔG~0)、焓变(ΔH~0)和熵变(ΔS~0)值均大于0,这表明草炭土对PCB138的吸附是一个非自发,吸热且吸附体系的混乱度增大的过程。该研究可为探讨PCBs在不同类型土壤中的环境行为提供一些基础数据,为PCBs的污染控制提供理论依据。     

菜园土壤铜吸附—解吸特性的研究

研究了菜园土壤铜的吸附－解吸特性。结果表明，３种菜园土壤吸附Ｃｕ＾２＋的量均随平衡液中Ｃｕ＾２＋浓度的增加而增大，可用Ｌａｎｇｍｕｉｒ方程和Ｆｒｅｕｎｄｌｉｃｈ方程来描述，由Ｌａｎｇｍｕｉｒ方程求得的菜园土壤对Ｃｕ＾２＋的最大吸附量和最大缓冲容量的大小顺序为：黄松土〉江涂土〉粉泥土，菜园土壤对Ｃｕ＾２＋的解吸量和解吸率均随其吸附量的增加而增加，吸附量与解吸量之间呈显著或极显著线性正相关。     

牛粪生物炭对紫色土吸附-解吸腐殖酸的影响

通过探讨牛粪生物炭对紫色土吸附-解吸腐殖酸的影响,以减少紫色土腐殖酸的流失、提高腐殖酸利用率,为提高龙川江流域紫色土肥力提供理论依据.采用土培实验,用Langmuir和Freundlich模型、Lagergren准一级和Lagergren准二级动力学方程,研究了不同添加比例牛粪生物炭(BC、CK、1%、3%、5%)对腐殖酸的吸附与解吸的影响.采用扫描电镜、BET等方法分析牛粪生物炭的表面结构以及比表面积,来探讨牛粪生物炭对紫色土吸附和解吸HA的影响机理.结果表明,牛粪生物炭对紫色土等温吸附HA过程符合Langmuir模型,动力学模型符合Lagergren准二级动力学方程;各处理对紫色土等温吸附-解吸HA过程有明显的影响,CK对HA的吸附量和吸附率最低,解吸率最高;5%对HA的吸附量、吸附率和解吸量最高.同时,各处理对紫色土吸附-解吸HA动力学也有明显的影响,在前12 h,吸附速率逐渐增加,随后吸附逐渐达到平衡,吸附过程以化学吸附为主.各处理方法相比,5%更有利于吸附HA,防止HA流失.     

磷对褐土中锌镉次级吸附和解吸影响

通过吸附和解吸试验,研究了不同磷吸附量石灰性褐土对锌镉次级吸附和解吸的影响。结果表明,次级吸附锌和镉对不同吸附量磷土壤的磷解吸量随磷吸附量的增加而增加,而磷解吸量随次级吸附后锌、镉浓度的增加而降低,即随锌镉添加量的增加,磷的有效性有所降低。土壤对锌的次级吸附量和吸附率随磷吸附量的增加先降低后升高,并随添加镉浓度的增加而降低,解吸量和解吸率随磷吸附量的增加而增加,说明在正常施磷范围内,增加磷的施用量能提高土壤中锌的有效性,同时,土壤对高浓度锌的次级吸附率小于低浓度锌的次级吸附率,而土壤对高浓度锌的解吸量和解吸率要远大于对浓度锌的解吸量和解吸率;土壤对镉的次级吸附量、吸附率和解吸量、解吸率都随着磷吸附量的增加而增加,且吸附量随添加镉的量增加而增加,但镉次级吸附量和吸附率随添加锌浓度的增加而减小,解吸量和解吸率却增大,说明在磷吸附量相同的条件下,添加锌促进了镉的有效性。     

硝磺草酮在黑土和红壤中的吸附-解吸特性

采用批量平衡实验,研究了硝磺草酮在黑土和红壤中吸附-解吸行为.结果表明,硝磺草酮在两种土壤中的吸附分为快速线性分配和慢速吸附两个阶段,2 h后,基本达到动态平衡.然而,其吸附速率随时间的延长而降低,且初始浓度和土壤性质对硝磺草酮吸附速率的变化率没有明显影响.硝磺草酮在红壤和黑土中吸附和解吸过程均能用Freundlich模型进行很好的拟合,拟合系数R2分别为0.999和0.993(黑土)、0.991和0.962(红壤).硝磺草酮在土壤中的吸附等温线呈现"L"型,以物理性吸附为主.硝磺草酮在两种土壤上的解吸过程存在一定的滞后现象,且随着硝磺草酮初始浓度增加,其解吸等温线的滞后系数也随之降低.黑土中硝磺草酮的吸附和解吸滞后强度均大于红壤.     

东北污灌区草甸棕壤吸附重金属铅的形态分布及解吸行为

以沈阳市沈抚污灌区的草甸棕壤为模型土,采用Tessier顺序提取法分析了吸附重金属Pb(Ⅱ)在土壤中的化学形态分布特点,研究了吸附Pb(Ⅱ)的解吸行为,特别考察了冷冻对吸附Pb(Ⅱ)化学形态分布及解吸行为的影响.研究表明,吸附Pb(Ⅱ)在东北草甸棕壤上的化学形态分布规律为:可交换态碳酸盐结合态铁锰氧化物结合态有机结合态残渣态;吸附Pb(Ⅱ)的解吸动力学过程可分为快速和慢速两个阶段,符合准二级动力学方程;冷冻对吸附Pb(Ⅱ)的形态分布基本无影响,而对平衡解吸率有明显影响,随冷冻时间延长,平衡解吸率逐渐降低;随pH值减小,平衡解吸率增大;pH值在5—10范围内,平衡解吸率变化幅度相对很小,而pH值低于5后,平衡解吸率急剧增大.随离子强度增大,平衡解吸率先急剧上升,后趋于平缓.提出Pb(Ⅱ)在东北草甸棕壤上的吸附机理:化学吸附和静电吸附,后者又可分为静电键合吸附和离子交换吸附.在实验条件下,静电吸附约占75%,化学吸附约占25%.     

Phenanthrene adsorption by soils treated with humic substances under different pH and temperature conditions

The mobility of phenanthrene (PHE) in soils depends on its sorption and is influenced by either the existing soil humus or exogenous humic substances. Exogenous humic acids (HAs) were added to soil to enhance the amount of soil organic carbon (SOC) by 2.5, 5.0, and 10.0 g kg⁻¹. PHE desorption of the treated soils was determined at two pH levels (3.0 and 6.0) and temperatures (15 and 25 °C). Soil PHE adsorption was related to pH and the type and quantity of added HAs. Humic acid (HA) and fulvic acid (FA) derived from peat had different effects on adsorption of PHE. Adsorption increased at first and then decreased with increasing quantity of exogenous FA. When the soil solution pH (in 0.005 M CaCl₂) was 4.5 or 3.0, the turning points were 2.5 g FA kg⁻¹ at pH 3.0 and 5 g FA kg⁻¹ at pH 4.5. When soil solution pH was 6, the amount of adsorbed PHE was enhanced with increasing exogenous HAs (HA or FA) and amount of adsorption by soil treated with FA was higher than with HA. Adsorption of PHE in the FA treatment at 10.0 g kg⁻¹ was lower than the controls (untreated soil or treatment with HAs at 0 g kg⁻¹) when the soil solution pH was 3.0. This suggests that FA adsorbed by soil was desorbed at low pH and would then increase PHE solubility, and PHE then combined with FA. PHE adsorption was usually higher under lower pH and/or lower temperature conditions. PHE sorption fitted the Freundlich isotherm, indicating that exogenous humic substances influenced adsorption of phenanthrene, which in turn was affected by environmental conditions such as pH and temperature. Thus, exogenous humic substances can be used to control the mobility of soil PAHs under appropriate conditions to decrease PAH contamination.     

碱性条件下胡敏酸吸附镉的特征研究

为了探讨胡敏酸在碱性条件下的吸附镉机理,了解碱性盐化土壤中镉污染机理和生态环境之间的关系,实验研究了胡敏酸在碱性条件吸附镉的特征。采用批吸附试验方法,研究不同Cd初始浓度、反应时间、不同pH和离子强度对胡敏酸吸附镉的影响,结果表明：胡敏酸具有较强吸附镉的能力,可以用Langmuir吸附模型和Temkin吸附模型很好地拟合其等温吸附过程（r分别为0.9809和0.9816）;在60 min内的快速反应阶段和60 min至6 h间的慢速反应阶段,胡敏酸对镉的吸附量分别为2.895 mg·g-1和3.342 mg·g-1,吸附反应平衡前6 h的动力学过程可以用Elovich方程进行很好的拟合（r为0.9285）;随着pH增加,吸附率表现出逐步增加趋势,并以pH为4.5和8.5为界,呈现两端增加速度快,中间增加慢的规律性;在较低浓度离子强度下,离子强度的增加促进胡敏酸吸附镉;而在高离子强度下,表现出相反的规律性;在相同的条件下,不同离子强度对胡敏酸吸附镉的影响大小为：氯化钙〉氯化镁〉氯化钾〉氯化钠。土壤在盐化的过程中,由于无机盐浓度的增加,增加了重金属离子的生物可利用性,加大了重金属离子的生态风险。     

沙土不同有机组分对磷的解吸特征影响

采用平衡解吸法研究了沙土不同有机组分对磷的解吸附特征影响。结果表明,通过过氧化氢去除有机质后的沙土使磷的解吸比例（Dr=0.94）大幅度增加,解吸迟滞性指数（TⅡ=0.05）显著降低;有机质是影响磷在沙土上解吸特征的重要因素;磷在橡胶态胶体（轻组有机组分）上的表面分配作用吸附是导致解吸比例（Dr=0.81）增大,解吸迟滞性指数（TⅡ=0.05）减小的原因;稳结态腐殖质中的胡敏酸在对磷的吸着和滞留过程中发挥重要作用,HⅡ＋HⅢ组（Dr=0.57、TⅡ=0.30）;磷在紧结态腐殖质所形成的团聚体结构中引起的团聚体结构不可逆形变是导致磷的解吸比例（HⅢ组Dr=0.24）降低,解吸迟滞性指数（HⅢ组TⅡ=0.49）增大的根本原因,考查土壤磷的解吸特征不但要考虑有机质的含量,更要考虑有机质的存在形态,它也是影响土壤磷解吸特征的重要因素,轻组有机组分、重组有机组分、以及重组有机组分中的稳结态腐殖质、紧结态腐殖质所携载的吸附态磷进入水体后对上覆水体的释放通量可分别按其饱和吸附量的81%、66%、57%和24%进行估算。     

改性腐殖酸对铀的吸附的试验研究

通过静态吸附实验,探讨了改性HA对U(Ⅵ)吸附影响。考查pH值、时间、U(Ⅵ)的初始浓度和温度等对吸附的影响。结果表明:pH值对改性腐殖酸的吸附效果影响较大,改性腐殖酸吸附U(Ⅵ)的最佳pH值为6,最大去除率为99.37%,吸附在60 min内基本达到平衡。UO22+在改性腐殖酸上的吸附是放热过程,符合Freundlich等温吸附方程,相关系数达0.99以上,表明IHA对铀的吸附是以表面为主要吸附位,并不是均匀的单层吸附。图8,参9.     

Effect of co-existing organic compounds on adsorption of perfluorinated compounds onto carbon nanotubes

Co-existing organic compounds may affect the adsorption of perfluorinated compounds (PFCs) and carbon nanotubes in aquatic environments. Adsorption of perfluorooctane sulfonate (PFOS), perfluorooctane acid (PFOA), perfluorobutane sulfonate (PFBS), and perfluorohexane sulfonate (PFH_xS) on the pristine multi-walled carbon nanotubes (MWCNTs-Pri), carboxyl functionalized MWCNTs (MWCTNs-COOH), and hydroxyl functionalized MWCNTs (MWCNTs-OH) in the presence of humic acid, 1-naphthol, phenol, and benzoic acid was studied. Adsorption kinetics of PFOS was described well by the pseudo-second-order model and the sorption equilibrium was almost reached within 24 h. The effect of co-existing organic compounds on PFOS adsorption followed the decreasing order of humic acid>1-naphthol>benzoic acid>phenol. Adsorbed amounts of PFOS decreased significantly in the presence of co-existing or preloaded humic acid, and both adsorption energy and effective adsorption sites on the three MWCNTs decreased, resulting in the decrease of PFOS adsorption. With increasing pH, PFOS removal by three MWCNTs decreased in the presence of humic acid and phenol. The adsorbed amounts of different PFCs on the MWCNTs increased in the order of PFBSxS相似文献   

风沙土不同有机组分对氨氮的解吸特征影响

采用平衡解吸法研究了风沙土不同有机组分对氨氮的解吸特征影响。结果表明,去除腐殖质后的风沙土氨氮解吸比例增加（由0.58增加到0.68）,同时,解吸迟滞性指数显著降低（由0.067降低到0.021）,说明腐殖质是影响风沙土氨氮解吸特征的重要因素;氨氮在轻组有机组分上的表面分配作用吸附是导致解吸比例增大,解吸迟滞性指数减小的原因;重组有机组分中的紧结态腐殖质（胡敏素）对氨氮的解吸起关键作用,它不但解吸比例较低（Dr=0.23）,而且解吸迟滞性指数较大（TⅡ=0.458）;氨氮在紧结态和稳结态腐殖质所形成的团聚体颗粒微孔隙中的不可逆吸附是导致解吸比例降低、解吸迟滞性指数增大的根本原因;考查土壤对氨氮的解吸特征不但要考虑有机质的含量,更要考虑有机质的存在形态,它也是影响土壤氨氮解吸特征的重要因素,轻组有机组分、重组有机组分及重组有机组分中的稳结态加紧结态腐殖质（HⅡ＋HⅢ组）和紧结态腐殖质（HⅢ组）携载的吸附态氨氮进入水体后,对上覆水体的扩散通量可分别按其饱和吸附量的0.94、0.58、0.33和0.23倍估算。     

Adsorption of humic acid from aqueous solution on bilayer hexadecyltrimethyl ammonium bromide-modified zeolite

Surfactant-modified natural zeolites (SMNZ) with different coverage types were prepared by loading hexadecyltrimethyl ammonium bromide (HTAB) onto the surface of a natural zeolite. The adsorption behavior of humic acid (HA) on SMNZ was investigated. Results indicate that the adsorbent SMNZ exhibited a higher affinity toward HA than the natural zeolite. HA removal efficiency by SMNZ increased with HTAB loading. Coexisting Ca²⁺ in solution favored HA adsorption onto SMNZ. Adsorption capacity decreased with an increasing solution pH. For typical SMNZ with bilayer HTAB coverage, HA adsorption process is well described by a pseudo-second-order kinetic model. The experimental isotherm data fitted well with the Langmuir model. Calculated maximum HA adsorption capacities for SMNZ with bilayer HTAB coverage at pH 5.5 and 7.5 were 63 and 41 mg·g^-1, respectively. E2/E3 (absorbance at 250 nm to that at 365 nm) and E4/E6 (absorbance at 465 nm to that at 665 nm) ratios of the residual HA in solution were lower than that of the original HA solution. This indicates that the HA fractions with high polar functional groups, low molecular weight (MW), and aromaticity had a stronger tendency for adsorption onto SMNZ with bilayer HTAB coverage. Results show that HTAB-modified natural zeolite is a promising adsorbent for removal of HA from aqueous solution.     

己唑醇在土壤中的吸附-解吸特性

采用批量平衡法和气相色谱法研究了己唑醇在3种土壤中的吸附-解吸特性.结果表明,己唑醇在3种供试土壤中的等温吸附-解吸曲线能较好地符合Freundlich模型,其吸附常数(Kf)分别为0.791、2.274和43.800,显示3种土壤吸附行为存在较大差异.吸附率与土壤有机质含量(OM)、土壤阳离子交换量(CEC)和粘粒含量呈良好相关性.己唑醇在粘土和壤土中的等温吸附线属于L型等温吸附线,砂土中属S型.己唑醇在土壤中的吸附自由能为-5.186—-8.164 kJ.mol-1,表示吸附机理主要为物理吸附.     

First determination of Cu adsorption on soil humin

Humic substances are heterogeneous mixtures of organic compounds occurring in huge amounts mainly in waters, soils, sediments and organic wastes. They are formed during the decay of living organisms. They play a very important role in many environmental processes including carbon sequestration, water cleaning and retention, soil erosion, fertility and pollutant retention. However, due to their complex nature, humic substances are still poorly characterized and much less known than living matter. Humin is the most insoluble and, in turn, the least understood fraction of humic substances. To our knowledge, no information is currently available on the adsorption and desorption behaviors of metal ions on soil humin. Here, we report the adsorption and desorption properties of Cu(II) on humin and humic acids isolated from a forest soil in northeast China using the batch equilibration method. Solid-state ¹³C cross-polarization magic angle spinning nuclear magnetic resonance (¹³C CPMAS NMR) spectroscopy was used to characterize and compare the chemical structures of humin and humic acid. The batch experiments’ results show that humin has a lower adsorption capacity and higher adsorption reversibility for Cu(II) than humic acid. The adsorption isotherms well fitted both the Langmuir and Freundlich equations. Humin, therefore, plays an important role in controlling the fate, transport and bioavailability of Cu(II) in the environment. The ¹³C CPMAS NMR spectra showed that compared with humic acid, humin was higher in alkyl C, carbohydrate C and phenolic C and was lower in methoxyl C, aryl C and carbonyl C. These findings mean that humin was less alkylated, more aliphatic and more hydrophobic.     

聚苯乙烯树脂吸附水中磺基水杨酸的研究

研究了两种聚苯乙烯树脂对水中磺基水杨酸的吸附行为，同时探讨了氨基修饰聚苯乙烯树脂的吸附动力学特性．结果表明，在所研究的磺基水杨酸浓度范围内，Langmuir和Freundich吸附等温方程都能很好地描述吸附平衡数据．采用氨基修饰制备的NDA-900树脂具有较大的吸附容量和较快的吸附速率，吸附动力学符合Lagergren二级速率方程，颗粒内扩散是NDA-900树脂吸附磺基水杨酸速率的主要控制步骤，可采用HSDM模型加以描述．