首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到19条相似文献,搜索用时 234 毫秒
1.
三种铁氧化物的磷吸附解吸特性以及与磷吸附饱和度的关系   总被引:17,自引:0,他引:17  
采用三种人工合成铁氧化物(针铁矿、赤铁矿和水铁矿)比较了结晶态和无定形铁氧化物对磷的吸附—解吸特性以及与磷吸附饱和度的关系。结果表明,三种铁氧化物的磷吸附特性均可用Langumir方程来描述,相关系数均大于0.9,达到极显著水平。从磷最大吸附量(Qm)、吸附反应常数(K)和最大缓冲容量(MBC)三项吸附参数综合考虑,水铁矿(无定形)对磷的吸附无论在容量还是强度方面均比结晶态铁氧化物针铁矿和赤铁矿大得多。水铁矿吸附的磷比针铁矿和赤铁矿所吸附的磷更难解吸;水铁矿的大量活性表面并没有表现出增加磷释放的作用。磷吸附饱和度有望作为评价土壤或铁氧化物磷吸附—解吸的强度和容量因子的一个综合指标。  相似文献   

2.
有机阴离子对磷酸根吸附的影响   总被引:50,自引:5,他引:50  
在中性条件下,低浓度的柠檬酸、草酸、酒石酸和胡敏酸阴离子都能显著降低针铁矿、非晶氧化铝、高岭石和红壤对磷酸根的吸附,尤其在低磷吸附饱和度下效果更好。有机阴离子抑制磷酸根吸附的能力因有机酸的种类和性质、以及固相的表面特性而异。有机阴离子存在下吸附的磷酸根具有较高的同位素32P交换活性和解吸率。测定了吸附平衡溶液中铁和铝的浓度。结果表明,在实验条件下(pH 7.0),即使较高浓度的有机酸根(10-2mol)也只能溶解极少量的铁和铝。有机阴离子络溶作用不足以说明固相吸附磷能力的显著下降。可见,有机阴离子降低磷酸根吸附的机制主要是竞争专性吸附。有机阴离子占据了一部分高亲和力的吸附位,从而降低了土壤固相吸附磷的量,增加了吸附态磷的活性。  相似文献   

3.
磷酸根在矿物表面的吸附-解吸特性研究进展   总被引:3,自引:0,他引:3  
严玉鹏  王小明  胡震  王慧  殷辉  刘凡  冯雄汉 《土壤》2021,53(3):439-448
综述了磷酸根在一些常见土壤矿物表面吸附–解吸特性的研究进展。磷酸根在矿物表面的吸附特性受环境pH、离子强度、温度、反应时间、矿物类型等多种因素的共同影响。一般说来,矿物表面的磷吸附量随pH降低而增加,受离子强度的影响较小。磷酸根在矿物表面的吸附动力学过程可分为快速吸附过程和慢速吸附过程,且在弱结晶矿物中存在微孔扩散过程。磷酸根在矿物表面的解吸过程通常存在两个阶段(初始快速解吸和随后的缓慢解吸),在解吸反应后期甚至还会发生再吸附。此外,磷酸根的吸附特性也受共存阴离子配体或金属阳离子的影响。其中,共存阴离子通过位点竞争、静电作用和空间位阻效应等机制影响磷酸根的吸附。天然有机质(包括胡敏酸和富里酸)降低了磷酸根在矿物表面的吸附,特别是在低p H条件下。通常,富里酸比胡敏酸更能有效降低磷酸根在矿物表面的吸附。金属阳离子可通过表面静电效应、形成三元络合物以及形成表面沉淀等机制促进磷酸根和金属在矿物表面的共吸附。最后,展望了与磷酸根在矿物表面吸附特性有关的研究热点和方向。  相似文献   

4.
有机酸根与铝氧化物表面吸附磷的解吸   总被引:7,自引:0,他引:7  
研究了有机酸根离子与合成铝氧化物表面吸附磷解吸的相互关系。结果表明:(1)有有机酸时比无有机酸时吸附的磷具有更高的解吸率,无草酸且加磷pH为4时,0.01molL-1KCI对磷的解吸率最低,草酸与磷共存且pH为6时磷的解吸率最高;(2)高浓度有机酸可解吸低浓度有机酸难解吸的磷,草酸难解吸的磷可为等浓度的柠檬酸极解吸;(3)不同浓度草酸和柠檬酸对铝-草酸复合物吸附磷的解吸率比对Al(OH)x的低,而对铝-柠檬酸复合物吸附磷的解吸率则比对Al(OH)x的高;(4)柠檬酸对铝-磷复合物中磷的解吸量随柠檬酸浓度升高而增大。这些结果证明,有机酸对铝氧化物吸附磷的解吸机理包括配位交换和溶解,有机酸可促进磷的解吸,提高磷的有效性。  相似文献   

5.
柠檬酸对三种人工合成氧化铁磷吸附特性的影响   总被引:1,自引:0,他引:1  
试验采用了3种人工合成的氧化铁为材料,研究了氧化铁对磷的吸附以及柠檬酸对氧化铁磷吸附特性的影响。结果表明:3种人工合成的氧化铁对磷的吸附特性及柠檬酸对氧化铁吸附磷的影响都可用Langumir方程来描述,都达到了极显著水平。从磷的最大吸附量(Sm)、吸附反应常数(K)和最大缓冲容量(MBC)来看,未加入柠檬酸时,水铁矿对磷的吸附在容量和强度方面均为最高;而在加入柠檬酸时,3种人工合成的氧化铁对磷的吸附能力的顺序并无差别,水铁矿和针铁矿的磷Sm和MBC要比赤铁矿大很多。  相似文献   

6.
周敏  徐则林  刘新  杜辉辉 《土壤》2022,54(4):810-816
本研究选取代表性层状硅酸盐蒙脱石,两种代表性氧化铁(水铁矿、针铁矿),合成蒙脱石-水铁矿、蒙脱石-针铁矿二元复合体,通过宏观吸附以及光谱学技术探究钨(WO42-)在蒙脱石-氧化铁复合体上的吸附行为和潜在机制。结果表明:氧化铁紧密覆盖在蒙脱石表面,使表面颗粒更加细小;钨的吸附量随pH升高而降低,3种吸附剂对钨吸附量大小顺序为:蒙脱石-水铁矿>蒙脱石-针铁矿>蒙脱石;原位红外光谱实验表明,钨在蒙脱石表面主要以外圈络合物形式存在,而在蒙脱石-氧化铁复合体上形成内圈络合物(Fe-O-W),且在低pH时,形成聚合态钨;X-射线光电子能谱进一步表明,针铁矿和水铁矿表面铁羟基参与了钨的络合反应。本研究证实,氧化铁覆盖不仅增大蒙脱石对钨的吸附量,而且使钨由外圈络合物形态转变为内圈络合态,进一步生成聚合态钨。研究结果对预测钨在土壤中的迁移转化、生物有效性和归宿有重要指导意义。  相似文献   

7.
结合吸附实验和X光吸收精细结构光谱(XAFS)分析,研究了草酸根和胡敏酸对As(V)在红壤中吸附的影响,分析了As(V)在红壤中的化学形态和微观结构以及草酸根、胡敏酸的影响特征。结果表明,当pH6.0时,红壤主要是通过基团交换反应吸附As(V),草酸根和胡敏酸可以通过竞争吸附位点抑制红壤中As(V)的吸附,其抑制作用随浓度增大而增强。XAFS光谱学数据表明,红壤中吸附的砷以+5价态存在,主要与铁铝矿物形成以约0.317 nm As-Al和0.328 nm As-Fe原子间距为特征的双齿双核结构的内层复合物,复合物结构类型不受砷浓度和草酸根、胡敏酸的影响。  相似文献   

8.
有机酸对铝氧化物吸附磷的影响   总被引:11,自引:1,他引:10  
以存在不同配位阴离子 (硫酸根、磷酸根、草酸根、柠檬酸根 )时合成的铝氧化物为对象 ,用平衡吸附法研究了草酸、柠檬酸等的浓度和 pH对铝氧化物吸附磷的影响 ,并讨论有机酸影响磷吸附的机制。结果表明 :六种合成铝氧化物的最大吸磷量 (Xm)介于 0.189~ 0.838mmol/g ,以Al(OH)x的吸磷量最高 ,铝 柠檬酸复合物 (Al-CA)的吸磷量最低 ;有机酸浓度升高时 ,铝氧化物的吸磷量降低 ,且柠檬酸的影响程度高于草酸 ;先加 pH为 2的草酸或酒石酸 ,Al(OH)x对磷的次级吸附量最低 ,而有机酸pH为 3时 ,Al(OH)x对磷的次级吸附量达最高 ,有机酸溶液 pH由 4增至 9,铝氧化物吸磷量变化不大或逐渐降低。有机酸与磷混合加入同单加磷相比 ,pH 3时差异较小 ,pH 4~ 6时差异最显著 ,pH 7~ 8时又减小 ;有机酸降低铝氧化物吸磷量的机理包括酸性溶解和络合竞争两方面 ,在 pH 2时以前者为主 ,pH 3~ 9时以后者为主 ,且铝氧化物表面的吸附点位对供试配位阴离子都是亲合的  相似文献   

9.
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。  相似文献   

10.
基于不同分析方法研究磷酸根在矿物表面吸附机制的进展   总被引:2,自引:1,他引:2  
磷素是植物生长必需的营养元素,也是联系生态系统中生物与非生物作用的关键元素。对磷酸根在矿物表面吸附反应机制的深入认识,有助于了解其在陆地和水环境中的形态、迁移、转化和生物有效性。本文主要综述了磷酸根在常见(土壤)矿物表面吸附机制的研究进展。各种分析技术或方法,如OH–释放量分析、Zeta电位分析(电泳迁移率测试)、等温滴定量热法、原子力显微镜、X射线光电子能谱、红外光谱、核磁共振波谱、X射线吸收光谱、表面络合模型、量子化学计算等,均以不同方式揭示磷酸根在不同矿物体系的吸附机制。磷酸根在矿物(尤其是铁、铝氧化物)表面的吸附通常伴随着水基和羟基的交换。一般认为磷酸根在矿物表面主要形成双齿双核、单齿单核内圈络合物,且受pH的影响较大。pH以及磷酸根在矿物表面的吸附密度影响内圈络合物的质子化状态。在低pH、高磷浓度、较高反应温度、较长吸附时间,以及弱晶质矿物吸附等条件下矿物表面吸附的磷可在矿物表面转化形成含磷的表面沉淀,造成矿物溶解转化以及磷生物有效性的进一步降低。最后展望了磷酸盐在矿物-水界面吸附有关的研究热点和方向。  相似文献   

11.

Purpose

The phosphate adsorption on natural adsorbents is of particular importance in regulating the transport and bioavailability of phosphates in environmental system. In soils, oxides are often associated with organic matter and form mineral-organic complexes. The aim of the present paper was to investigate the mechanisms of phosphate adsorption on these complexes.

Materials and methods

Phosphate adsorption on uncoated and humic acid (HA)-coated iron oxide complexes was investigated at different ionic strengths and pH by isotherm experiments and attenuated total reflectance Fourier transform infrared (ATR-FTIR) spectroscopy.

Results and discussion

Results showed that HA-coated iron oxide complexes caused a decrease in the specific surface area (SSA) and the isoelectric point (IEP) of oxides. Phosphate adsorption on iron oxides was insensitive to changes of ionic strength, while it increased on the complexes with increasing ionic strength. The presence of HA decreased the maximum adsorption and the affinity of phosphate on the complexes. The zeta potential of phosphate-bound iron oxides linearly reduced with the increment of phosphate surface coverage, while the zeta potential of complexes with adsorbed phosphate kept at the same level. ATR-FTIR analysis suggested the formation of phosphate-metal complexation. The presence of HA promotes the formation of the monodentate phosphate complexes at pH 4.5 and significantly influenced phosphate species at pH 8.5.

Conclusions

The amount of phosphate adsorbed was reduced, and the phosphate speciation was also influenced when phosphate was adsorbed on HA-coated iron oxide complexes compared with phosphate adsorption on pure goethite and hematite.
  相似文献   

12.
磷酸盐在水铁矿及水铁矿-胡敏酸复合体表面的吸附   总被引:3,自引:1,他引:3  
The adsorption of phosphate onto ferrihydrite (FH) and two FH-humic acid (HA) complexes, obtained by co-precipitating FH with low (FH-HA1) and relatively high amounts of humic acid (FH-HA2), was studied through kinetics and isotherm experiments to determine the differences in phosphate adsorption between FH-HA complexes and FH and to reveal the mechanism of phosphate adsorption onto two soil compositions. The isoelectric point (IEP) and the specific surface area (SSA) of the mineral decreased as the particle porosity of the mineral increased, which corresponded to an increase in the amount of organic carbon. The adsorption capacity of phosphate was higher on FH than on FH-HA1 and FH-HA2 at the scale of micromoles per kilogram. The initial adsorption rate and adsorption affinity of phosphate decreased with an increase in the amount of HA in the mineral. The sensitivity of phosphate adsorption to the change in the pH was greater for FH than for FH-HA complexes. Ionic strength did not affect the adsorption of phosphate onto FH and FH-HA1 at a lower pH, and the increase in the ionic strength promoted phosphate adsorption at a higher pH. However, for the FH-HA2 complex, the increase in the ionic strength inhibited the adsorption of phosphate onto FH-HA2 at a lower pH and increased the adsorption at a higher pH.  相似文献   

13.
Competition in adsorption between humic acid (HA) or fulvic acid (FA) and phosphate on synthetic goethite, gibbsite and two tropical soils was studied. The results for both goethite and gibbsite showed that HA and FA competed strongly with phosphate for adsorption sites at low pH values. The soils showed a similar result with a reduction in phosphate adsorption resulting from the addition of HA at the pH of the soils. The competition between HA and phosphate at different pH levels is illustrated by comparing the adsorption envelopes for phosphate on goethite, gibbsite and the two soils in the presence and absence of HA. The trends observed may be explained by the relative positions of the maximum buffer-power (buffer capacity) of the organic acids and of phosphoric acid which are shown to lie in different pH ranges.  相似文献   

14.
Abstract

Selenite adsorption by a variety of oxides consisting of iron (Fe), aluminum (Al), titanium (Ti), manganes (Mn), and silicon (Si), and by two humic acids were investigated in order to grasp selenite behavior and fixation mechanisms in soil. It was found that selenite was apparently adsorbed even by the Mn oxides on which surface negative charge was dominant in normal pH range (pH <4). No selenite adsorption was observed in the silicon dioxide (SiO2) and the two humic acids. A sequential extraction of adsorbed selenite with competitive anions showed the differences of binding force or stability of adsorbed selenite among the minerals. While the goethite fixed selenite strongly, selenite adsorbed on the Mn oxide was easily released to the liquid phase with other anions, such as phosphate. Each mineral had its inherent characteristic in ligand exchange reactions accompanied with selenite sorption. Selenite sorption by the Mn and the Ti oxides resulted in large increase of surface negative charge, while only a little increase in the Fe and Al oxides. Proton consumption with selenite sorption was extremely smaller for the Mn oxide than for the others.  相似文献   

15.
磷酸盐吸附对可变电荷土壤正负电荷的影响   总被引:9,自引:1,他引:9       下载免费PDF全文
赵安珍  张效年 《土壤学报》1997,34(2):123-129
本文研究了华南地区不同类型的可变电荷土壤,并对磷酸盐的吸附量和吸附磷后土壤的正、负电荷的变化,以及pH和游离氧化铁对这种变化的影响进行了研究。结果表明,土壤吸磷量与土壤游离氧化铁含量成良好的正相关。土壤吸磷后正电荷减少,负电荷增加,土壤电荷量与吸磷量之间呈抛物线状相关。吸附1摩尔磷酸盐对土壤净负电荷的贡献在0.3-1.0摩尔之间。土壤中的游离氧化铁使吸附的磷对土壤负电荷的贡献减少。  相似文献   

16.
风化煤腐殖酸对氮、磷、钾的吸附和解吸特性   总被引:16,自引:1,他引:16  
研究了风化煤腐殖酸在不同pH值条件下对氮、磷、钾的吸附和解吸特性。结果表明,1)在pH.4~8条件下,随着氮、磷、钾初始处理浓度的增加,腐殖酸对其吸附量和解吸量均呈上升趋势,但解吸率均呈下降趋势;2)在不同pH值的介质溶液中,腐殖酸对氮、磷、钾的吸附和解吸特性不尽相同,其中,在碱性条件下,腐殖酸对氮的吸附和解吸作用较强,在酸性条件下,腐殖酸对磷的吸附和解吸作用较强,而腐殖酸对钾的的吸附和解吸作用在中性条件下更易发生;3)腐殖酸对氮、磷、钾的等温吸附可用Linear、Langmuir和Freundlich三个吸附方程来拟合,相关性达显著或极显著水平,但以Freundlich方程为最优。  相似文献   

17.
Low‐molecular‐weight (LMW) organic acids exist widely in soils, especially in the rhizosphere, and the adsorption of these acids may affect their reactions in soils. The adsorption behaviour of phthalic acid and salicylic acid by two variable charge soils (a Rhodic Ferralsol and a Haplic Acrisol) was investigated. Both soils exhibited great adsorption capacity for these organic acids, with a greater affinity for phthalic acid. The Rhodic Ferralsol adsorbed more organic acids of both kinds than the Haplic Acrisol, which was consistent with the content of iron and aluminum oxides in the two soils. The iron oxides in these soils played a significant role in adsorption of the organic acids, whilst the soil aluminosilicate minerals, such as kaolinite, showed a small adsorption capacity. The presence of phosphate and sulphate caused a decrease in the adsorption of both organic acids because of their competition with them for sorption sites. The phosphate showed a bigger inhibition on the adsorption than sulphate as a result of a greater amount of phosphate adsorbed by the soils. The adsorption of both organic acids was affected by pH only slightly at pH < 4.5. However, the adsorption decreased with the increase in pH at pH > 4.5. A similar trend was observed for the phosphate system, but the opposite was seen for the sulphate system. This suggests that the inhibition of sulphate on the adsorption of the organic acids decreased with the increase in pH, because the adsorption of sulphate decreased strongly with increasing pH.  相似文献   

18.
【目的】腐殖酸对磷肥增效的调控效应与其结构性密切相关。本文比较了不同磺化反应方法制备的腐殖酸磷肥对冬小麦磷素利用的影响,为制备调控磷肥专用的腐殖酸增效载体提供依据。【方法】采用磷酸与氢氧化钾反应法制备普通磷肥 (P)、普通腐殖酸磷肥 (HAP),并采用加双氧水、硝酸等方法制备了四种磺化腐殖酸磷肥 (HA1P、HA2P、HA3P和HA4P)。用田间土柱栽培试验方法,在等磷量基础上,设置普通磷肥 (P)、普通腐殖酸磷肥 (HAP)、磺甲基化腐殖酸磷肥 (HA1P)、双氧水+磺甲基化腐殖酸磷肥 (HA2P)、硝酸+磺甲基化腐殖酸磷肥 (HA3P)、双氧水+硝酸+磺甲基化腐殖酸磷肥 (HA4P) 6个处理,同时设置不施磷肥对照 (CK) 处理和施用等量腐殖酸处理 (C-HA、C-HA1、C-HA2、C-HA3、C-HA4)。调查了小麦产量和产量构成及经济效益,分析了0—80 cm土壤有效磷含量。【结果】1) 与CK相比,普通腐殖酸 (C-HA) 和磺化处理腐殖酸 (C-HA1、C-HA2、C-HA3、C-HA4) 对小麦籽粒产量无显著影响。与P处理比较,HAP、HA1P、HA2P、HA3P、HA4P处理的小麦籽粒产量分别提高了6.3%、17.8%、10.1%、17.5%、11.1%,4个腐殖酸磺化磷肥 (HA1P、HA2P、HA3P、HA4P) 处理均高于普通腐殖酸磷肥 (HAP) 处理。2)与HAP比较,磺化腐殖酸磷肥处理HA1P、HA2P、HA3P、HA4P分别提高小麦地上部磷吸收量12.3%、12.3%、9.2%、10.8%,其中HA1P和HA2P处理最高。3)与HAP比较,磺化腐殖酸磷肥处理HA1P、HA3P分别提高小麦磷肥农学效率23.6%和7.1%。4)与HAP比较,磺化腐殖酸磷肥处理HA1P、HA2P、HA4P可分别提高0—20 cm土层土壤速效磷含量17.5%、16.2%、17.2%。【结论】磺化腐殖酸磷肥比普通腐殖酸磷肥可以更有效地提高土壤中磷肥的有效性,提高冬小麦对磷素的吸收利用,进而提高冬小麦籽粒产量。四种磺化工艺中,以磺甲基化处理的腐殖酸磷肥 (HA1P) 效果最优。  相似文献   

19.
The adsorption of three s-triazines (atrazine, terbutylazine, and simazine) on three different humic acids (HAs), before and after acidic hydrolysis, was studied at four diverse pH values from 3 to 4.5. The Freundlich sorption affinity (K(f)) and intensity (1/n) of s-triazines were related to the chemical and structural composition of HA and used in a multivariate statistical analysis. At low pH, the sorption values for s-triazines were not directly justified by the content of carboxyl groups in original HA, while only an increase of phenolic carbons in hydrolyzed HA supported the increased s-triazine adsorption. The structural composition of both s-triazines and humic samples explained 86% of the significance in multivariate analyses, whereas the role of pH remained hidden in only 14% of the statistical significance. Adsorption of s-triazines was mainly related to carbon content, hydrophobicity, and aromaticity of HA, thereby implying a predominant binding role of weak dispersive forces. Steric properties explained the larger adsorption affinity of atrazine and terbutylazine with respect to simazine. The occurrence of charge-transfer interactions between atrazine and mainly hydrolyzed HA was further suggested by the increased number of free radicals detected in atrazine-HA complexes at different pH values. Charge-transfer interactions were postulated to occur when HA conformations became progressively controlled by aromatic components. This work indicates that humic matter rich in hydrophobic and aromatic constituents is more likely to adsorb s-triazines and reduce their environmental mobility.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号