氧化还原条件对湿地土壤磷吸附与解吸特性的影响

采用室内模拟试验研究了氧化还原条件对盘锦天然湿地土壤磷吸附与解吸特性的影响,并对磷的吸附与解吸过程进行拟合。结果表明,氧化或还原条件下Langmuir模型和Freundlich模型均能较好地拟合磷的等温吸附曲线,且Langmuir方程的拟合效果好于Freundlich方程。淹水还原条件下,湿地土壤对磷的最大吸附量和解吸率比淹水前分别降低了9.5%和16.3%;吸附解吸平衡浓度升高,平均增加158.8%。淹水后土壤活性铁含量明显升高,淹水前后活性铁变化与吸附解吸平衡浓度变化之间的相关性达到了显著水平,与土壤中磷的最大吸附量和解吸率变化的相关性不显著,表明活性铁含量的变化是淹水还原条件下影响土壤磷吸附解吸平衡浓度变化的主要因素。     

紫色土中砷、磷的吸附-解吸和竞争吸附

采用批培养法研究了As、P在三峡库区典型土壤紫色土中的吸附-解吸特点及竞争吸附对As、P迁移活化的影响.结果表明：3种紫色土中As、P的吸附-解吸特点相似,等温吸附均符合Langmuir和Freundlich方程,As在酸性、中性和石灰性紫色土中的最大吸附量分别为1428.6、1250.0和1111.1 mg·kg^-1;P在酸性、中性和石灰性紫色土中的最大吸附量分别为322.6、357.1和434.8 mg·kg^-1;As、P吸附动力学过程为先快后慢,均符合一级动力学方程与Elovich方程,快速吸附段符合一级动力学方程,为交换吸附;慢速吸附阶段满足Elovich方程,可能属于深层吸附或专性吸附.As、P竞争吸附试验表明,As、P共存时P的吸附速度和吸附量均增强,而As的吸附速度和吸附量均降低,表明As的存在能明显增强紫色土对P的吸附作用,P的存在则明显抑制紫色土对As的吸附.     

退耕还湖后湿地土壤对磷的吸附解吸特性

以安徽菜子湖区不同退耕年限(3、5、9和11年)湿地为研究对象,以相邻油菜地和原始湿地为对照(共6个样地),研究退耕还湖后湿地土壤对磷的吸附解吸特性变化.结果表明: 退耕湿地土壤对磷的等温吸附曲线与Langmuir和Freundlich吸附方程拟合程度均达极显著水平(P<0.01);6个样地土壤对磷的最大吸附量(X_m)、吸附常数(K)和最大缓冲容量(MBC)范围分别为478～1074 mg·kg^-1、0.14～0.61和68.6～661.5 mg·kg^-1,且退耕湿地的这些参数均随着退耕年限的延长而升高,但未达到原始湿地水平;6个样地土壤磷的平均解吸率为6.2%～14.6%,且退耕湿地土壤磷解吸率随着退耕年限的延长呈先增高后降低的趋势,但均显著高于原始湿地.表明随着退耕年限的增加,湿地土壤对外源磷的固持能力不断增强,而土壤有机质和粘粒含量是影响湿地土壤对外源磷固持能力的重要因子.     

湿地沉积物对磷的吸附-解吸动力学模型概述

介绍了常用的吸附-解吸动力学模型(Freundlich方程、Langmuir方程及Temkin模型),分析比较了不同模型之间的相互关系,对目前国内外关于磷吸附-解吸动力学模型研究进行了简要概述,介绍了不同模型的统一表达形式,并提出应加强对不同类型湿地中沉积物对磷的吸附-解吸过程及其动力学模型、对吸附-解吸过程的长期监测和不同环境因子间的交叉效应研究等建议,以深化对动力学模型的认识,从净化机理层面充分理解湿地生态系统的运行机制.     

不同污染负荷土壤中镉和铅的吸附－解吸行为

采用一次平衡法,对3种不同污染负荷土壤Cd2 和Pb2 的吸附-解吸行为进行了比较.结果表明,低污染负荷土壤对Cd2 和Pb2 的吸附能力高于高污染负荷土壤.3种土壤对Cd2 的吸附等温线与Freundlich方程有较好的拟合性,Pb2 的等温吸附过程可用Langmuir方程与Freundlich方程来描述.双常数方程是描述这3种不同污染负荷土壤中Cd2 和Pb2 吸附动力学行为的最优模型,其次为Elovich方程,最差模型是一级动力学方程.Pb2 的解吸滞后现象较Cd2 明显.高污染负荷土壤的吸附态Cd2 、Pb2 解吸率高于低污染负荷土壤,Cd2 、Pb2 解吸量与其初始吸附量之间的关系符合二次幂方程.3种土壤Cd2 、Pb2 的解吸速率随重金属初始浓度的增加而增加,随解吸时间的延长而降低.     

泉州市不同利用方式下土壤磷的吸附与解吸特性

分析了不同利用方式下泉州市土壤磷素吸附-解吸特征.结果表明:Langmuir等温方程式可以很好地表征土壤磷素的吸附特性;旱地和轮作地土壤对磷的吸附能力较强,而草地和林地土壤对磷的吸附能力较弱;磷的流失风险顺序为轮作地＞草地＞林地＞旱地;指导施磷量与吸附常数、最大缓冲量的大小顺序一致,为旱地＞轮作地＞林地＞草地;轮作地和草地的解吸率高于旱地和林地,土壤的缓冲能力顺序为旱地＞林地＞轮作地＞草地.主成分分析表明,平均解吸率、易解吸磷、磷吸附指数和磷零吸持平衡浓度4个指标最能反映土壤磷素流失潜力,可作为评价流失潜力的主要指标.     

广东省主要母质发育水稻土对磷的吸附特性

对广东省5种不同母质上发育的水稻土进行了P素等温吸附试验.结果表明,供试土壤的等温吸附数据与Langmuir、Freundlich和Temkin 3个方程都能很好地拟合,但以Langmuir方程拟合程度最好(相关系数从0.995^**到0.999^**).利用Langmuir方程计算的P最大吸附量(Xm)和吸附强度因子(K)的乘积(KXm:P吸附特性值)可以作为水稻土吸附P素的综合指标,KXm的大小可以表明水稻土施P次序.试验结果还表明供试水稻土对P素吸附存在两种不同的吸附区.     

不同粒径生物炭对土壤磷吸附-解吸特性的影响

粒径是影响物质吸附性能的一个重要因素。本研究以不同粒径(0.25～1 mm、0.075～0.25 mm、<0.075 mm)油菜秸秆生物炭(SBC)和鸡粪生物炭(MBC)分别与两种土壤(高磷土、低磷土)混合进行室内培养30 d,通过土壤磷等温吸附试验与解吸试验，结合土壤磷吸附相关性质，评价不同粒径生物炭对土壤磷吸附-解吸特性的影响。结果表明：在水体系中，3个粒径的SBC与MBC对磷的吸附能力大小均表现为<0.075 mm(43125、20083 mg·kg^-1)>0.075～0.25 mm(37376、13199 mg·kg^-1)>0.25～1 mm(27749、12251 mg·kg^-1);在土壤体系中，同一种生物炭的3个粒径间土壤磷吸附量差异较小。与无生物炭处理相比，添加SBC提高了土壤对磷的最大吸附量(S_max),增幅为236.8%～755.7%,并降低了土壤磷解吸率；添加MBC的S_max增幅较SBC低，但提高了土壤磷解吸率(增幅为7.2%～295...     

低磷石灰性土壤施磷和小麦秸秆后土壤微生物量磷的变化

通过室内培养试验,向低磷的石灰性土壤加入磷(0、25、50、100 mg P·kg^-1,KH₂PO₄)和小麦秸秆(5 g C·kg^-1),25 ℃下培养90 d,研究在施肥和秸秆还田条件下土壤微生物量磷及微生物含磷量的变化特点,及其与土壤有效磷之间的关系.结果表明：土壤微生物量磷、微生物含磷量随加入无机磷量的提高而增加,最高分别为71.37和105.34 mg·kg^-1;除非加入足够的无机磷(如100 mg·kg^-1),否则同时加入秸秆会降低土壤微生物量磷和微生物含磷量,这种效果在培养初期更加明显.土壤微生物量磷和微生物含磷量与土壤有效磷之间存在显著的正相关关系（相关系数R²分别为0.26和0.40,n=49）.加入的无机磷可迅速转化为微生物量磷,表观贡献率最高可达71%,秸秆的加入可使表观贡献率进一步提高.     

择伐干扰对小兴安岭阔叶红松林土壤磷吸附解吸的影响

以小兴安岭地区阔叶红松林经过轻度、中度和强度择伐干扰后形成的天然林以及未经干扰的原始林(对照)林地表层(0～10 cm)土壤为对象,对土壤磷素的最大吸附量、吸附强度、最大缓冲容量、最大解吸量、平均解吸率和易解吸磷量等指标进行测定,研究不同干扰强度导致土壤磷吸附解吸的规律性变化,分析择伐干扰对阔叶红松林土壤磷吸附解吸特征的影响.结果表明: 各林地土壤磷最大吸附量为1383.93～1833.34 mg·kg^-1,中度和强度干扰林地显著高于轻度干扰林地和原始林地;磷吸附强度为0.024～0.059 L·mg^-1,强度和轻度干扰显著增加了林地土壤磷吸附强度;最大缓冲容量为35.68～97.97 L·kg^-1,强度干扰林地土壤的最大缓冲容量最高.择伐干扰显著降低了林地土壤的供磷潜力.各样地土壤磷最大解吸量、平均解吸率和易解吸磷量分别为526.32～797.54 mg·kg^-1、14.7%～25.5%和1.79～5.41 mg·kg^-1,林地土壤磷素释放能力随干扰强度的增加显著降低.择伐干扰通过降低林地土壤磷的供应及释放能力改变了阔叶红松林土壤磷吸附与解吸特征.     

Thermodynamic and kinetic studies for environmentaly friendly Ni(II) biosorption using waste pomace of olive oil factory

The objective of this study is to assess the environmentaly friendly Ni(II) adsorption from synthetic wastewater using waste pomace of olive oil factory (WPOOF). Batch kinetic studies were performed in order to investigate the adsorbent and adsorbate dose, solution pH, agitating speed and temperature. The maximum Ni(II) adsorption was obtained at pH 4.0. The equilibrium nature of Ni(II) adsorption at different temperature was described by the Freundlich, Langmuir and Temkin isotherms. The equilibrium data fit well the Temkin and Langmuir isotherm. The monolayer adsorption capacities of WPOOF as obtained from Langmuir isotherm at 60 °C was found to be 14.80 mg/g. The adsorption mechanism was examined by the FTIR technique. The results of the thermodynamic investigations indicated that the adsorption reactions were spontaneous (ΔG < 0), slightly endothermic (ΔH > 0) and irreversible (ΔS > 0). The pseudo first-order, pseudo second-order, Elovich and intraparticle diffusion kinetic models were used to describe the kinetic data.     

镉在黑土和棕壤中吸附行为比较研究

比较研究了重金属镉在黑土和棕壤中的吸附热力学和动力学行为.结果表明,在实验设定的浓度范围内,黑土和棕壤对Cd²⁺吸附量随溶液中Cd²⁺浓度的增加而增加.黑土对Cd²⁺的吸附固定能力明显强于棕壤.在平衡液浓度为20 mg·kg^-1时,黑土对Cd²⁺的吸附量为1 485.2 mg·kg^-1、棕壤为700.6 mg·kg^-1.两种土壤对Cd²⁺的吸附等温线与Langmuir、Freundlich和Henry方程均有较好的拟合性,而Temkin方程不适合用来描述Cd²⁺在两种土壤中的等温吸附.根据Langmuir的拟合结果,Cd²⁺在黑土和棕壤中的最大吸附量分别可达5 939.3和2 790 mg·kg^-1.黑土较高的吸附能力与其高的有机质含量和粘粒含量有关.黑土和棕壤中Cd²⁺的吸附是一个快速反应过程,2 min内能达到平衡吸附量的90%,15～30 min左右达到吸附平衡.一级动力学方程是拟合Cd²⁺在黑土和棕壤中吸附动力学过程的最优方程,其次为Elovich方程和双常数方程.随着初始浓度的增加,Cd²⁺在土壤中的吸附速率也不断增大.随着吸附量的增大和反应时间的延长,吸附速率不断下降.在较低的初始浓度下,Cd²⁺在黑土中的下降趋势要快于棕壤.     

小分子有机酸对恒电荷土壤胶体Pb2＋吸附-解吸的影响

供试土壤胶体对Pb²⁺吸附及吸附态Pb²⁺的解吸等温线均符合Freundlich和Langmuir等温式,吸附常数Ka值大小为塿土>黄绵土>黑垆土>黄褐土,其大小次序与表面总电荷密度σ0大小一致,表明了各土壤胶体对Pb²⁺吸附强度的大小,在小分子有机酸作用下,吸附量降低,吸附亲和力增加,柠檬酸的影响大于草酸的影响;解吸后残留Pb^2+吸附常数杨值的大小基本为塿土>黄褐土>黑垆土>黄绵土,反映了解吸残留Pb²⁺吸附强度的大小,与各土壤胶体有机质和游离氧化铁含量有关,在NaNO₃和草酸溶液中,吸附-解吸等温线相距较远,吸附-解吸之间存在着滞后性;在柠檬酸作用下,吸附-解吸等温线基本接近,二者之间具有一定的可逆性。     

Reactions of boron with soils

Boron is an essential micronutrient for plants, but the range between deficient and toxic B concentration is smaller than for any other nutrient element. Plants respond directly to the activity of B in soil solution and only indirectly to B adsorbed on soil constituents. Soil factors affecting availability of B to plants are: pH, texture, moisture, temperature, organic matter and clay mineralogy. Boron adsorbing surfaces in soils are: aluminium and iron oxides, magnesium hydroxide, clay minerals, calcium carbonate, and organic matter. Boron adsorption reactions can be described empirically using the Langmuir adsorption isotherm equation, the Freundlich adsorption isotherm equation, and the phenomenological Keren model. Chemical models such as the constant capacitance model, the triple layer model, and the Stern VSC-VSP model can describe B adsorption over changing conditions of solution pH and B concentration. Boron desorption reactions often exhibit hysteresis. The rate of B desorption can be described using the first order rate equation, the Elovich reaction rate equation, and the power function equation.     

Prediction of fertilizer phosphate requirement using the Langmuir adsorption maximum

The phosphate adsorption maximum as calculated by the Langmuir equation was used to predict the fertilizer P requirement of wheat (Triticum aestivium, cv. Caldwell) on both virgin and cultivated Decatur clay loam (clayey, kaolinitic, thermic, Rhodic Paleudult) and Hartsells sandy loam soils (fine-loamy, siliceous, thermic, Typic Hapludult). Soils with higher adsorption maximum were found to require more fertilizer P than soils with lower adsorption maximum. For soils 25% saturation of the adsorption maximum gave the optimum dry matter yield. This corresponded to equilibrium P concentration of 0.45 mg L⁻¹ for Decatur cultivated and 0.31 mg L⁻¹ for Decatur and Hartsells virgin soils for optimum dry matter yield. These values are within the range of those reported previously by other investigators working with different soils.     

Adsorption kinetics,isotherm, and thermodynamics studies of acetyl-11-keto-β-boswellic acids (AKBA) from Boswellia serrata extract using macroporous resin

An acetyl-11-keto-β-boswellic acid (AKBA) is potent anti-inflammatory agent found in Boswellia serrata oleogum resin. Adsorption characteristics of AKBA from B. serrata were studied using macroporous adsorbent resin to understand separation and adsorption mechanism of targeted molecules. Different macroporous resins were screened for adsorption and desorption of AKBA and Indion 830 was screened as it showed higher adsorption capacity. The kinetic equations were studied and results showed that the adsorption of AKBA on Indion 830 was well fitted to the pseudo first-order kinetic model. The influence of two parameters such as temperature (298, 303, and 308?K) and pH (5–8) on the adsorption process was also studied. The experimental data was further investigated using Langmuir, Freundlich, and Temkin isotherm models. It was observed that Langmuir isotherm model was found to be the best fit for AKBA adsorption by Indion 830 and highest adsorption capacity (50.34?mg/g) was obtained at temperature of 303?K. The values of thermodynamic parameters such as the change of Gibbs free energy (ΔG*), entropy (ΔS*), and enthalpy (ΔH*), indicated that the process of adsorption was spontaneous, favourable, and exothermic.