土壤
土壤
토양
SOILS
2010年
2期
280-287
,共8页
王涛%余贵芬%王芳%卞永荣%王聪颖%蒋新
王濤%餘貴芬%王芳%卞永榮%王聰穎%蔣新
왕도%여귀분%왕방%변영영%왕총영%장신
菲%单宁酸%无定形铝氧化物%回归方法%吸附等温线
菲%單寧痠%無定形鋁氧化物%迴歸方法%吸附等溫線
비%단저산%무정형려양화물%회귀방법%흡부등온선
Phenanthrene%Tannic acid%Al (oxy)hydroxides%Regression methods%Sorption isotherms
采用批实验研究了菲在单宁酸干扰下形成的不同晶形铝氧化物上的吸附现象,并用不同的吸附等温线方程对吸附平衡数据进行了拟合,重点比较了线性和非线性回归方法估计吸附等温线参数的差异.结果表明:菲在各种晶形的铝氧化物上都有明显的吸附,但并不是完全随着单宁酸含量和结晶度的变化而规律性变化.吸附平衡数据以Langmuir、Redlich-Peterson和Dubinin-Radushkevich吸附等温方程,用不同的回归方法估计的等温线参数值均有显著性差异.线性回归得到的参数有不确定性,表明用线性回归来判断吸附等温线能否对吸附平衡数据进行最优拟合是不可靠的.相反,非线性回归能较好地确定菲在不同晶形铝氧化物上的最佳吸附等温线及相应参数.采用R2和x2共同检验发现,菲在4种不同结晶度(单宁酸与铝的摩尔比(MR)=0,10-3,10-2,10-1)铝氧化物上的最佳吸附等温线方程并不尽相同,分别为Freundlich,Freundlich,Dubinin-Radushkevich和Freundlich,反映了各种晶形的铝氧化物的表面异质性.修正的Freundlich方程比较不同晶形铝氧化物对菲的相对吸附容量顺序为:MR=10-3<MR=10-2<MR=0<MR=10-1.由此,认为菲在无定形铝氧化物上的吸附是熵驱动的结果.
採用批實驗研究瞭菲在單寧痠榦擾下形成的不同晶形鋁氧化物上的吸附現象,併用不同的吸附等溫線方程對吸附平衡數據進行瞭擬閤,重點比較瞭線性和非線性迴歸方法估計吸附等溫線參數的差異.結果錶明:菲在各種晶形的鋁氧化物上都有明顯的吸附,但併不是完全隨著單寧痠含量和結晶度的變化而規律性變化.吸附平衡數據以Langmuir、Redlich-Peterson和Dubinin-Radushkevich吸附等溫方程,用不同的迴歸方法估計的等溫線參數值均有顯著性差異.線性迴歸得到的參數有不確定性,錶明用線性迴歸來判斷吸附等溫線能否對吸附平衡數據進行最優擬閤是不可靠的.相反,非線性迴歸能較好地確定菲在不同晶形鋁氧化物上的最佳吸附等溫線及相應參數.採用R2和x2共同檢驗髮現,菲在4種不同結晶度(單寧痠與鋁的摩爾比(MR)=0,10-3,10-2,10-1)鋁氧化物上的最佳吸附等溫線方程併不儘相同,分彆為Freundlich,Freundlich,Dubinin-Radushkevich和Freundlich,反映瞭各種晶形的鋁氧化物的錶麵異質性.脩正的Freundlich方程比較不同晶形鋁氧化物對菲的相對吸附容量順序為:MR=10-3<MR=10-2<MR=0<MR=10-1.由此,認為菲在無定形鋁氧化物上的吸附是熵驅動的結果.
채용비실험연구료비재단저산간우하형성적불동정형려양화물상적흡부현상,병용불동적흡부등온선방정대흡부평형수거진행료의합,중점비교료선성화비선성회귀방법고계흡부등온선삼수적차이.결과표명:비재각충정형적려양화물상도유명현적흡부,단병불시완전수착단저산함량화결정도적변화이규률성변화.흡부평형수거이Langmuir、Redlich-Peterson화Dubinin-Radushkevich흡부등온방정,용불동적회귀방법고계적등온선삼수치균유현저성차이.선성회귀득도적삼수유불학정성,표명용선성회귀래판단흡부등온선능부대흡부평형수거진행최우의합시불가고적.상반,비선성회귀능교호지학정비재불동정형려양화물상적최가흡부등온선급상응삼수.채용R2화x2공동검험발현,비재4충불동결정도(단저산여려적마이비(MR)=0,10-3,10-2,10-1)려양화물상적최가흡부등온선방정병불진상동,분별위Freundlich,Freundlich,Dubinin-Radushkevich화Freundlich,반영료각충정형적려양화물적표면이질성.수정적Freundlich방정비교불동정형려양화물대비적상대흡부용량순서위:MR=10-3<MR=10-2<MR=0<MR=10-1.유차,인위비재무정형려양화물상적흡부시적구동적결과.
A batch experiment was conducted to study the sorption of phenanthrene onto AI (oxy)hydroxides formed under the influence of tannic acid. The sorption isotherms were employed to describe the sorption behavior. Linear and nonlinear regression methods were compared to select the optimal isotherm. Results showed that significant sorption of phenanthrene occurred on the surfaces of all A1 (hydro)oxides, but the sorption capacity didn't completely conform with tannic acid content and crystal form. Results generated with linear regression showed some uncertainties,indicating that linear regression was not good to determine the best fitting isotherm. In contrast, nonlinear regression was found to be better to obtain the parameters involved in the isotherms and also the optimal isotherm. By comparing R2 and x2 values, the optimal isotherm for sorption of phenanthrene onto different AI (oxy)hydroxides with different tannic acid/Al molecular ratios (MRs=0, 10-3 ,10-2, 10-1 ) were Freundlich, Frenndlich,Dubinin-Radushkevich and Frenndlich isotherm, respectively, which implied the heterogeneity of Al (oxy) hydroxides surfaces. Modified Freundlich isotherm was adopted to compare directly phenanthrene sorption characteristics of different Al (oxy)hydroxides formed under the influence of tannic acid and found the sorption capacity increasing with the order of MR=10-3<MR=10-2<MR=O<MR=10-1. We deduced that phenanthrene sorption is entropy-driven.