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Chemical Species of Aluminum Ions in Acid Soils 被引量:7
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作者 XURENKOU JIGUOLIANG 《Pedosphere》 SCIE CAS CSCD 1998年第2期127-133,共7页
INTRODUCTIONAluminumtoxicityisoneofthemainfactorslimitingplantgrowthonacidsoils.Aluminumfromacidsoilsisamaj... INTRODUCTIONAluminumtoxicityisoneofthemainfactorslimitingplantgrowthonacidsoils.AluminumfromacidsoilsisamajorsourceofAlinsur... 展开更多
关键词 酸性土壤 铝离子 PH值 毒性 化学形态
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Effect of Electrolyte on the Dissolution of Aluminum from Acid Soils and the Distribution of Aluminum Forms inSoil Solution
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作者 XURENKOU JIGUOLIANG 《Pedosphere》 SCIE CAS CSCD 1997年第4期331-338,共8页
KCl, CaCl2, NH4Cl, NaCl, K2SO4 and KF solutions were used for studying the effects of canons and anions on the dissolution of aluminum and the distribution of aluminum forms respectively. Power of exchanging and relea... KCl, CaCl2, NH4Cl, NaCl, K2SO4 and KF solutions were used for studying the effects of canons and anions on the dissolution of aluminum and the distribution of aluminum forms respectively. Power of exchanging and releasing aluminum of four kinds of canons was in the decreasing order Ca2+ >K+ >NH+4 >Na+.The dissolution of aluminum increased with the canon concentration. The adsorption affinity of various soils for aluminum was different. The aluminum in the soil with a stronger adsorption affinity was difficult to be exchanged and released by canons. The Al-F complexes were main species of inorganic aluminum at a low concentration of canons, while Al3+ became major species of inorganic aluminum at a high concentration of canons. The results on the effect of anions indicated that the concentrations of total aluminum, three kinds of inorganic aluminum (Al3+, Al-F and Al-OH complexes) and organic aluminum complexes (Al-OM)when SO2-4 was added into soil suspension were lower than those when Cl- was added. The dissolution of aluminum from soils and the distribution of aluminum forms in solution were edicted by the adsorption of Fon the soil. For soils with strong affinty for F- , the concentrations of the three inorganic aluminum species in soil solution after addition of F- were lower than those after addition of Cl-; but for soils with weak affinity for F- , the concentrations of Al3+ and Al-OM were lower and the concentrations of Al-F complexes and total inorganic aluminum after addition of F- were higher than those after addition of Cl-. The increase of F- concentration in soil solution accelerated the dissolution of aluminum from soils. 展开更多
关键词 酸性土壤 铝离子 种类 分解 电解流 毒性 植物生长
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Sequential Extraction of Aluminum and Iron from Acidic Soils by Chemical Selective Dissolution Methods 被引量:1
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作者 HEJIZHENG A.VIOLANTE 《Pedosphere》 SCIE CAS CSCD 1998年第1期37-44,共8页
Potassium chloride, Na-pyrophosphate, CuCl2, NH4-oxalate, dithionite-citrate-bicarbonate (DCB) and Na-citrate solutions were employed to extract aluminum (Al) and iron (Fe) sequentially and separately from 15 acidic s... Potassium chloride, Na-pyrophosphate, CuCl2, NH4-oxalate, dithionite-citrate-bicarbonate (DCB) and Na-citrate solutions were employed to extract aluminum (Al) and iron (Fe) sequentially and separately from 15 acidic soils located at the Mangshan Mountains, Hunan Province, China. Many evidences showed that separate pyrophosphate extracted mainly KCI-extractable Al, organo-Al complexes and some inorganic Al compounds, whereas separate CuCl2 extracted KCl-extractable Al and some organo-Al complexes. CuCl2 extracted much less amounts of Al than pyrophosphate did from the soils. Separate oxalate did not extract all KCl-Pyrophosphate- CuCl2 -oxalate sequentially extractable Al and Fe. Also, separate DCB did not extract all KCl- pyrophosphate- CuCl2 -oxalate- DCB sequentially extractable Al. The forms of Al extracted by oxalate and DCB from the soils were majorly noncrystalline. The interlayered materials of 1.4-nm intergrade minerals of the soils were attributed mainly to hydroxy Al polymers. 展开更多
关键词 酸性土壤 赋存形态 化学选择性分解方法 萃取 湖南
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Effects of Tannic Acid on Active Aluminum Species Distribution in Various Tea Soils
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作者 You-Jian Su Wan-You Liao +3 位作者 Ye-Jun Wang Yong-Li Zhang Yi Luo Shan-Guo Hu 《茶叶》 2013年第4期299-307,共9页
Effects of tannic acid on active aluminum species distribution in different pH tea soils in Yunnan and Jiangxi tea gardens were studied by field observation and laboratory analysis.There were 4 species of active alumi... Effects of tannic acid on active aluminum species distribution in different pH tea soils in Yunnan and Jiangxi tea gardens were studied by field observation and laboratory analysis.There were 4 species of active aluminum in the tea soil,i.e.,exchangeable aluminum Al3 +,unimer hydroxyl aluminum Al(OH)2 +Al(OH)+2,acid-soluble aluminum Al(OH)03and humic-acid aluminum Al-HA.Experimental results showed that tannic acid at levels 0 ~0.4 mmol/kg and 0 ~ 2.0 mmol/kg,with the rising of soil pH value,the content of exchangeable aluminum decreased significantly,hydroxyl aluminum,acid-soluble aluminum and humic-acid aluminum were increased gently.When the concentration of tannic acid increased to above 2.0 mmol/kg,the inhibition of higher concentration of tannic acid on content of active aluminum was strengthened with the rising of soil pH value and variation law of 20 ~ 40 cm soil layer was similar to 0 ~ 20cm soil layer.Generally speaking,the content of active aluminum in upper layer of soil were more than subsoil and total content of active aluminum in Yunnan tea soils were higher than Jiangxi tea soils.The correlation analysis showed that the soil pH were positively correlated with hydroxyl aluminum,humic-acid aluminum,pHBC(r = 0.796,0.960,0.852;p < 0.01,0.01,0.01) in 0 ~ 20cm soil layer.pHBC were significant negative correlated with exchangeable aluminum(r =- 904,p < 0.01),hydroxyl aluminum(r =- 645,p < 0.05),and with humic-acid aluminum have a positive correlation,correlation coefficient was0.795(P < 0.05).Meanwhile,the tannic acid addition concentration were 0 ~ 0.4 mmol/kg soils pH were increased significantly,while samples attains a peak pH value afterwards decrease continuously,the relationship between the pH and the concentration of tannic acids accords with the equation:Y pH=- 0.04C DN+3.82(R2= 0.95,P < 0.01).When the concentration of tannic acid up to about 8.0 ~ 12.0 mmol/kg,soil pH keep unchanged.Therefore,we can clearly draw that effects of tannic acid on active aluminum content of the inflection point is not the same in different region of tea garden soil.Low concentration tannic acid can improve the soil content of various forms of aluminum,but with the increase in the amount of tannic acid,the various forms of aluminum content are inhibited.With the soil pH increased,high concentrations tannic acid on the inhibition of the release of active aluminum increased.pH and tannic acid on the total amount of active aluminum garden soil was mutual weakening effect relationship. 展开更多
关键词 铝形态分布 土壤活性 茶园土壤 单宁酸 土壤PH值 浓度增加 实验室分析 交换性铝
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pH对酸性土壤中铝的溶出和铝离子形态分布的影响 被引量:97
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作者 徐仁扣 季国亮 《土壤学报》 CAS CSCD 北大核心 1998年第2期162-171,共10页
pH对酸性土壤中铝的溶出和土壤溶液中铝离子形态分布的影响的研究结果表明,土壤中铝的溶出量随pH降低而增加,pH对不同土壤中铝的溶出的影响不同,三种土壤中铝的溶出量受pH影响的大小顺序是:红壤>赤红壤>砖红壤,说明不同类型土壤... pH对酸性土壤中铝的溶出和土壤溶液中铝离子形态分布的影响的研究结果表明,土壤中铝的溶出量随pH降低而增加,pH对不同土壤中铝的溶出的影响不同,三种土壤中铝的溶出量受pH影响的大小顺序是:红壤>赤红壤>砖红壤,说明不同类型土壤中铝的溶出对外来酸的敏感程度不同。对三种单核无机形态铝的研究结果表明,土壤溶液中铝离子的形态分布随pH的改变而变化。随pH降低,Al3+占总单核无机铝的比例增加,而Al-F络合物呈相反的变化趋势,在所研究的pH范围内,Al-OH均占很小的比例,一般不超过总单核无机铝的5%。温度影响铝的溶出量和溶出的铝离子形态的分布,随着温度的降低,铝的溶出量增加,Al3+占无机铝的百分数增加,而Al-F络合物所占比例相应减小。土壤溶液中的聚合态铝占总酸溶性铝的比例随pH的降低而减小。在酸性至强酸性条件下(pH<45),聚合态铝所占比例很小。对红壤和砖红壤的研究结果表明,酸性土壤中铝的溶解度主要受固相铝的氧化物所控制。 展开更多
关键词 酸性土壤 铝溶出量 铝离子形态 PH
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不同集约栽培年限下雷竹林土壤化学性质与生理毒性铝的分布 被引量:11
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作者 李子川 庄舜尧 +3 位作者 桂仁意 季海宝 李国栋 郑康乐 《浙江农林大学学报》 CAS CSCD 北大核心 2011年第6期837-844,共8页
通过研究集约经营条件下,雷竹Phyllostachys praecox栽培时间对土壤化学性质,尤其是对土壤酸度和土壤生理毒性铝形态分布的影响,为评估酸化雷竹林地土壤铝毒胁迫强度及其在雷竹林土壤退化过程中的贡献提供理论支持。设对照(水稻田和红豆... 通过研究集约经营条件下,雷竹Phyllostachys praecox栽培时间对土壤化学性质,尤其是对土壤酸度和土壤生理毒性铝形态分布的影响,为评估酸化雷竹林地土壤铝毒胁迫强度及其在雷竹林土壤退化过程中的贡献提供理论支持。设对照(水稻田和红豆杉Taxus chinensis幼林地)和栽植年限分别为2,6(2009年冬天第1次覆盖),8,11,16和20 a(退化林地)的雷竹林地共8种/类样地(处理),每种(类)样地设3个采样样方,取样剖面分别为0~10,10~20和20~40 cm。结果表明:改植雷竹后,随着竹林栽培时间的延长,表层和亚表层土壤(0~10 cm和10~20 cm)酸碱度从对照的pH 6.53(水稻土)和pH 5.57(红豆杉幼林地)下降到pH 3.55(栽培20 a雷竹林地),土壤有机质和阳离子交换量在覆盖后逐渐上升,土壤腐殖质稳定性不断下降,而土壤电导率随竹林经营强度和施肥量的变化而呈前期上升后期下降的趋势。雷竹林表层和亚表层土壤(0~10 cm和10~20 cm)中8-羟基喹啉提取态铝质量分数随竹林栽培时间的延长和土壤酸度值的下降而增加,相比较于对照水稻田和红豆杉幼林地(10.08 mg.kg-1和22.94 mg.kg-1),栽培16 a后雷竹林土壤中8-羟基喹啉提取态铝质量分数高达108.01 mg.kg-1,分别高出对照(水稻土和红豆杉幼林地)10倍和5倍;雷竹林土壤中乙酸提取态铝与8-羟基喹啉提取态铝的变化趋势基本一致。相关分析表明:两者呈极显著正相关关系(r=0.911 7,P<0.000 1,校正后的R2=0.828 7)。以上结果说明:随着雷竹林集约经营时间的增加和土壤持续酸化,雷竹林地遭受铝毒胁迫的风险逐渐增加。 展开更多
关键词 土壤学 雷竹 集约经营 土壤化学性质 铝形态 生理毒性铝
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红壤粘粒对Co、Cu、Pb和Zn吸附亲和力的研究 被引量:58
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作者 王维君 邵宗臣 何群 《土壤学报》 CAS CSCD 北大核心 1995年第2期167-178,共12页
本文研究了高度风化的酸性红壤对Co、Cu、Pb、Zn离子的吸附特性。用吸附曲线形状,吸附方程,分配系数,pH_(50)值等讨论了吸附亲和力特征及其影响因素和吸附反应的机理。结果表明,红壤粘粒吸附重金属离子主要由Fe、... 本文研究了高度风化的酸性红壤对Co、Cu、Pb、Zn离子的吸附特性。用吸附曲线形状,吸附方程,分配系数,pH_(50)值等讨论了吸附亲和力特征及其影响因素和吸附反应的机理。结果表明,红壤粘粒吸附重金属离子主要由Fe、Al氧化物所控制。金属离子对红壤粘粒的吸附亲和力(以pH_(50)表示)主要决定于离子本身的化学性质,亲和力以Cu≥Pb>zn>Co顺序减少,易水解的离子吸附亲和力较大,亲和力也受土壤组分及其表面性质影响,含Fe、Al氧化物多的粘粒其表面的反应活性也较大,对金属离子的亲和力较强。通过竞争吸附方程对吸附-pH曲线的描述和分配系数等的讨论,揭示出四种离子与红壤粘粒的反应机理并不相同,Cu、Pb离子以专性吸附反应为主,Zn、Co则非专性吸附占一定比例。对专性吸附机理。 展开更多
关键词 酸性 红壤 重金属 吸附亲和力 吸附特性
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H^+和有机酸对可变电荷土壤铝释放的动力学研究 被引量:11
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作者 王代长 蒋新 +2 位作者 贺纪正 邓建才 卞永荣 《地球化学》 CAS CSCD 北大核心 2006年第6期651-659,共9页
利用流动搅动法研究了在模拟酸雨和低分子量有机酸条件下可变电荷土壤铝释放的动力学特征,结果表明,在pH3.5的模拟酸雨作用下,红壤和黄壤中流出液铝的浓度范围约为15~40μmol/L,铝的释放快反应来源于土壤交换性铝和有机络合态铝,铝的... 利用流动搅动法研究了在模拟酸雨和低分子量有机酸条件下可变电荷土壤铝释放的动力学特征,结果表明,在pH3.5的模拟酸雨作用下,红壤和黄壤中流出液铝的浓度范围约为15~40μmol/L,铝的释放快反应来源于土壤交换性铝和有机络合态铝,铝的释放慢反应对应于含铝矿物的溶解。赤红壤和砖红壤上在0~300min内流出液铝的浓度范围约为1~5μmol/L,流出液pH值大于4.5,对H+的缓冲作用表现为阳离子交换、SO24-的专性吸附释放OH-和矿物表面的质子化;当流出液pH值小于4.5时,H+开始溶解土壤中的含铝固相,铝释放的最后浓度为20~30μmol/L。用相近pH值的有机酸溶出土壤铝的浓度比pH3.5的模拟酸雨要高,特别是在砖红壤上,开始就有大量铝的释放,其浓度为20~75μmol/L,红壤上是70~150μmol/L,随时间延长,流出液中的铝浓度分别为10~20μmol/L和20~30μmol/L。有机酸作用下铝的释放机制主要是有机酸被土壤吸附后,有机酸与位于表面晶格中的铝原子形成络合体,促进了铝的溶解;其次是有机酸的吸附掩盖了土壤表面的质子化过程,增强了酸的溶解,以及有机配体对铝的络合作用,增加了铝的释放量。不同有机酸对铝的溶出能力也有不同,其释放铝能力的大小为:柠檬酸>酒石酸>苹果酸,这取决于有机配体与铝的络合能力。 展开更多
关键词 H^+离子 低分子量有机酸 铝释放动力学 可变电荷土壤
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pH、温度和水土比对酸性土壤溶液中铝离子形态分布的影响 被引量:9
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作者 徐仁扣 《热带亚热带土壤科学》 CSCD 1998年第1期26-30,共5页
溶液中Al3+、Al-F和有机络合态铝(Al-OM的浓度随pH降低而增加,Al3+在总单核铝中所占比例随pH的降低而增加,而Al-F络合物呈相反的变化趋势.土壤中铝的溶解度与土壤中铝氧化物的结晶形态有关,处于较高纬度地区的土壤,由于铝氧化物的... 溶液中Al3+、Al-F和有机络合态铝(Al-OM的浓度随pH降低而增加,Al3+在总单核铝中所占比例随pH的降低而增加,而Al-F络合物呈相反的变化趋势.土壤中铝的溶解度与土壤中铝氧化物的结晶形态有关,处于较高纬度地区的土壤,由于铝氧化物的结晶形态较差,在相同pH下,其铝的溶解度较大.土壤溶液中有机络合态铝的浓度随温度升高而增加,在pH不变的情况下,土壤中无机铝的溶解量随温度降低而增加.随水土比增加,土壤溶液中Al3+、Al-F络合物和Al-OM浓度减小,但按每kg土计算的铝溶解量随水土比的增加而增加. 展开更多
关键词 酸性土壤 铝离子形态 PH 温度 水土比
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土壤与酸的反应时间对土壤酸度及土壤溶液中铝离子形态分布的影响 被引量:1
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作者 徐仁扣 季国亮 《热带亚热带土壤科学》 CSCD 1998年第4期296-298,共3页
用两种土壤研究土壤与酸的反应时间对土壤酸度及土壤溶液中铝离子形态分布的影响。结果表明,土壤溶液pH随反应时间增加而增加,安徽红壤pH的增幅大于江西红壤。在pH3.0的HNO3溶液中,土壤溶液中的总铝及Al3+均随反应时间增加而减少,而... 用两种土壤研究土壤与酸的反应时间对土壤酸度及土壤溶液中铝离子形态分布的影响。结果表明,土壤溶液pH随反应时间增加而增加,安徽红壤pH的增幅大于江西红壤。在pH3.0的HNO3溶液中,土壤溶液中的总铝及Al3+均随反应时间增加而减少,而在pH3.5的HNO3溶液中,土壤溶液中总铝及Al-F络合物先随反应时间的增加而减小.然后又有所增加。 展开更多
关键词 反应时间 土壤酸度 铝离子形态 土壤溶液
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氟离子加入法区分强酸性矿质土壤溶液中无机单核铝的形态 被引量:2
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作者 徐仁扣 季国亮 《化学传感器》 1996年第3期179-184,共6页
本文介绍了区分强酸性矿质土壤溶液中无机单核铝离子的形态的氟离子加入法。向土壤溶液中加入一已知量的氟标准溶液,再用氟离子电极测定和区分溶液中无机单核铝的形态。实验结果表明,对有机质含量很少的强酸性矿质土壤溶液,用该方法测... 本文介绍了区分强酸性矿质土壤溶液中无机单核铝离子的形态的氟离子加入法。向土壤溶液中加入一已知量的氟标准溶液,再用氟离子电极测定和区分溶液中无机单核铝的形态。实验结果表明,对有机质含量很少的强酸性矿质土壤溶液,用该方法测定的不同形态无机单核铝的相对偏差<5%,说明该方法的测定结果可靠。从几种红壤的测定结果看,在强酸性土壤溶液中,Al^(3+)和AlF^(2+)是主要的无机单核形态。 展开更多
关键词 氟离子加入法 强酸性 土壤 铝离子 离子选择电极
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我国西南湖塘溪流的水化学组成与离子平衡的研究
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作者 孟宪林 周定 薛含斌 《四川环境》 北大核心 1996年第1期5-11,共7页
本文研究了我国重酸雨地区四川、贵州省湖塘溪流的水化学组成及离子平衡关系。结果表明:城郊之间水化学组成存在差异;同时,进行离子平衡衡算时,须对溶解态钙、镁进行校正,否则,会出现阴离子短缺现象.仅由钙、镁及硫酸根和弱酸根... 本文研究了我国重酸雨地区四川、贵州省湖塘溪流的水化学组成及离子平衡关系。结果表明:城郊之间水化学组成存在差异;同时,进行离子平衡衡算时,须对溶解态钙、镁进行校正,否则,会出现阴离子短缺现象.仅由钙、镁及硫酸根和弱酸根组成的简单离子平衡也是大致符合的,但其应用有一定的局限性。 展开更多
关键词 化学组成 离子平衡 游离态 溶解态 酸雨
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