酸性硫酸盐土中铝的形态

采用连续分级提取方法 ,把酸性硫酸盐土中可提取的非晶体态铝区分为交换态铝 (ExAl)、吸附态无机羟基铝 (HyAl)、有机配合铝 (OrAl)、氧化铁结合铝 (DCBAl)、层间铝 (InAl)和非晶体态铝硅酸盐 (NcAl) ,其平均值分别为 1.79、2 .5 1、4.17、4.14、4.31和 18.6 6g·kg-1Al2 O3.实际酸性硫酸盐土中NcAl>OrAl >InAl >DCBAl>ExAl>HyAl,潜在酸性硫酸盐土NcAl >InAl >DCBAl >HyAl >OrAl >ExAl.可提取Al总量平均为 35 .5 7Al2 O3g·kg-1,占全Al 2 5 .0 4% .其显著特征是活性铝ExAl、HyAl和OrAl的含量较高 .每一种Al形态的结构组成与酸性硫酸盐土相应性质和生态特性密切相关 .酸化的ASS的强酸环境导致Al的过量游离 ,并转化为活度较大的活性Al,从而产生Al毒     

酸性硫酸盐土中硫形态转化过程的水分制约作用

分别设土壤田间持水量的30%恒定(FH1)、土壤田间持水量的70%恒定(FH2),一直淹水(INU)、风干后放置(DRY,作为对照)、自然风干(NAD)5个处理进行酸性硫酸盐土室内模拟实验。实验结果显示,水分条件对酸性硫酸盐土中水溶性硫、交换性硫和黄铁矿硫的形态转化有显着的制约作用。淹水环境和过分干燥环境都不利于黄铁矿的氧化及水溶性硫和交换性硫的形成,潮湿但含水量不饱和环境有利于黄铁矿硫向水溶性硫和交换性硫的转换。模拟试验期内,水溶性硫含量的增加速度排列为:FH2>FH1>INU,交换性硫含量的增加速度排列为:FH1>FH2>INU,黄铁矿硫含量的下降速度排列为:FH2>FH1>INU,原状土自然风干(NAD)过程中,水溶性硫、交换性硫和黄铁矿硫之间发生了明显的转化。对不同处理中黄钾铁矾硫、有机硫和元素硫的动态变化也进行了分析。     

酸性硫酸盐土水改旱后土壤化学性状的变异初报

探讨了酸性硫酸盐水稻土改为旱作后土壤化学性状的变异以及比较不同利用方式之间的经济效益．结果表明,酸性硫酸盐水稻土改种甜玉米和蔬菜后,土壤化学性状发生显著变化．耕层土壤酸度、水溶性硫酸根含量、土壤活性铝和活性铁含量均显著降低．经济效益得到显著提高．建议对水改旱后的环境效应进行深入研究以及进行定位观测,以便合理利用这一特殊的土壤资源     

外源钾对铁胁迫下水稻细胞壁多糖含量及耐铁性的影响

以耐铁毒型水稻品种协优9308和铁毒敏感型水稻品种Ⅱ优838为实验材料,采用溶液培养法研究250mg.L-1Fe2+(EDTA-Fe2+)胁迫下,不同钾水平对两种水稻的生长特性、酸性磷酸酶(APA)、果胶甲酯酶(PME)、根系果胶含量、半纤维素1含量以及半纤维素2含量的影响。结果表明,经250mg.L-1Fe2+处理7d和14d后,协优9308和Ⅱ优838的相对根长明显下降,APA、PME的活性显著升高,果胶含量、半纤维素1含量、半纤维素2含量显著增加,Ⅱ优838酶活性及细胞壁多糖含量提高幅度较大,表现出其铁毒敏感性,并且随着处理时间的延长,铁胁迫对两种水稻相对根长,PME活性,HC1含量及HC2含量的影响越显著,但APA活性和果胶含量则没有明显变化。加入外源钾可以不同程度的降低酶活性及细胞壁多糖含量,外源钾浓度为200mg.L-1,对水稻相对根长,APA活性,HC1含量缓解效果较好;外源钾浓度为400mg.L-1,对PME活性,果胶含量缓解效果较好。随着外源钾浓度升高,水稻铁毒症状得到不同程度的缓解,但钾浓度高于200mg.L-1又会对水稻造成新的胁迫。由此推测,水稻通过提高根系细胞壁多糖含量来增加根尖铁的结合位点,以及细胞壁的厚度和刚性,并降低细胞壁的伸展性,使根细胞的伸长受抑,从而提高其铁耐性。     

三峡地区茶园土壤化学特征与茶叶品质的关系

 根据土壤地球化学分类原则,长江三峡地区主要植茶土壤为硅铝质铁铝土、钾硅质铁铝土和硅铁质铁铝土3种土壤地球化学类型。硅铝质铁铝土的特点是土壤质地粗,剖面分异明显,硅、铝、钾含量高,铁、钙、镁含量低：钾硅质铁铝土多为砂壤质,硅、钾含量较高;硅铁质铁铝土土层深厚,质地粘重,铁、铝含量高,磷、钾含量低。土壤地球化学特征与茶叶品质的关系至为密切。砂质土有利于提高茶叶氨基酸含量,而粘质土则会使氨基酸含量降低;较高的盐基含量会降低茶叶茶多酚、咖啡碱和水浸出物含量,但有利于氨基酸形成;速效磷与水浸出物成显著正相关,但与咖啡碱成显著负相关;缓效钾与氨基酸成正相关。从总体上看,硅铝质铁铝土上产出的茶叶品质较高,适宜植茶,硅铁质铁铝土上茶叶品质欠佳,如无特殊改良措施,不宜开辟为茶园。     

稻米镉积累的铁肥调控

以FeSO4和EDTA二钠亚铁（EDTA·Na2Fe,也称EDTA二钠铁）为铁肥,通过土施和叶片喷施研究不同形态铁肥及施肥方式对水稻（Oryza Sativa L．）镉积累的影响．结果显示不论施用何种形态铁肥或何种施用方式对水稻生长和产量性状均没有不利影响．土施EDTA·Na2Fe显著降低了水稻根系、地上部以及稻米（糙米和精米）中的镉含量,并且两基因型水稻精米中的镉含量远低于0．2mg／kg,达到国家限制标准．但土施FeSO4、叶面喷施FeSO4及叶面喷施EDTA·Na2Fe处理均显著增加了根系、地上部及稻米（糙米和精米）中的镉含量．结果还显示施用铁肥可显著提高稻米的铁、铜、锰含量,同时对锌含量也有影响．研究结果认为土施EDTA·Na2Fe等络合态亚铁肥,维持土壤中较高的有效态铁含量以及亚铁含量是控制稻米镉积累的一条新型可行途径．     

初始pH值对碱性和酸性水稻土微生物铁还原过程的影响

酸碱度(pH值)是水稻土铁还原过程的重要影响因素之一。通过模拟水稻土淹水厌氧培养,以Al2(SO4)3和Na2CO3溶液分别调节碱性和酸性水稻土pH值至强酸性(pH值5.0)、酸性(pH值5.0—6.5)、中性(pH值6.5—7.5)、碱性(pH值7.5—8.5)、强碱性(pH值8.5),以此来研究5种初始pH值对水稻土泥浆铁还原过程的影响;通过微生物群落厌氧培养研究了2种水稻土菌悬液在6种pH值条件下的铁还原能力差异。结果表明,碱性水稻土铁还原潜势(a)、最大铁还原速率(V max)随初始pH值的降低而下降,而达到最大铁还原速率所需的时间(T Vmax)则延长。提高酸性水稻土初始pH值使铁还原V max增加而T Vmax缩短,但土壤中无定形氧化铁均能还原,初始pH值与V max具有显著正相关关系。碱性和酸性水稻土的土壤菌悬液在试验pH值范围内厌氧培养,其铁还原能力在培养初期差异不显著,但培养后期的差异明显,且最终都能把培养液中氧化铁完全还原。随着初始pH值升高T Vmax延长,V max则降低,且均显著负相关,但碱性水稻土微生物群落的V max在pH值6.00时最大。初始pH值和土壤类型对水稻土铁还原过程具有显著影响,且对土壤菌悬液微生物群的铁还原具有一定影响。     

重金属在根际中的化学行为Ⅲ.土壤中铁形态转化的根际效应及其生态学意义

本文研究了两种熟化水稻土和两种新垦红壤植稻后根际中铁的形态转化。结果表明,水稻土植稻后根际中无定形铁、游离铁、络合态铁及铁的活化度均低于非根际;红壤中除络合态铁的根际内外分布趋势与水稻土相同外,其余均与水稻土相反。穆斯堡尔谱特征表明,根际中氧化铁的四极矩分裂较大,内磁场较低,即根际中氧化铁被活化。差热分析结果表明根际土的持水力强于非根际土。这对根际微生态系统的生态环境保护、物质流的调控及水分的保持和有效利用有重要作用。     

不同土壤水分条件下酸性硫酸盐土硫形态转化特征

以4种土壤湿度、3种干湿交替周期和原状土自然风干8个处理进行酸性硫酸盐土室内模拟实验,对模拟过程内土壤6种硫形态和pH等指标的动态变化过程的跟踪测定和分析结果表明,水分条件对酸性硫酸盐土中水溶性硫、交换性硫和黄铁矿硫的形态转化制约作用显著．淹水环境和过分干燥环境都不利于黄铁矿的氧化及水溶性硫和交换性硫的形成．潮湿但含水量不饱和环境有利于黄铁矿硫向水溶性硫和交换性硫的转换．在3种周期的干湿交替处理中,单一排干期水溶性硫和交换性硫土壤含量平均上升幅度分别为0．90～1．63g·kg^-1和0．58～1．47g·kg^-1,而黄铁矿硫含量下降幅度为1．29～3．20g·kg^-1．淹水期黄铁矿硫含量相对稳定而水溶性硫和交换性硫含量明显下降,并在排水过程中造成总硫的部分流失．硫形态转化量和硫的淋失量受到干湿交替周期的显著影响．同时分析了黄钾铁钒硫、有机硫和元素硫的动态．     

聚乙二醇模拟干旱对耐低钾水稻幼苗的根系生长及某些生理特性的影响

以早籼品种‘瑰宝八号’及其变异后代耐低钾的水稻为材料,用20%PEG6000模拟干旱,测定幼苗根系形态和部分生理特性的指标并对其抗旱能力进行比较的结果表明:耐低钾水稻幼苗的超氧化物歧化酶活性、根系活力和活跃吸收面积相对较高,而丙二醛含量相对较低,其根重和根体积也高,比其亲本‘瑰宝八号’有更高的抗旱能力.     

酸性硫酸盐土中硫的形态含量分布和酸化特征

对广东省台山市南部滨海平原酸性硫酸盐土(以下简称ASS)S的形态、含量、分布和酸化特征的研究表明,ASS全硫含量高达0.615%,比咸田高2～6倍,比砂泥田高3～9倍;其硫以无机硫为主,占全硫的82.3%～90.4%,其中,黄铁矿硫的含量最高,占全硫的30.3%～46.2%,黄铁矿硫在剖面中的分布与全硫含量同步。ASS硫含量的空间变异和剖面内部的分异十分显着。ASS发育过程中,适合黄铁矿累积的环境及其持续时间与地形地貌(山)的关系十分密切。ASS的主要致酸物质是黄铁矿的氧化,酸化的ASS的pH一般在5.5以下,最低达2.83.ASS可氧化总酸度一般比实际总酸度高2～3倍,潜在的环境风险极.     

Effects of hyper-enriched reactive Fe on sulfidisation in a tidally inundated acid sulfate soil wetland

Solid phase Fe and S fractions were examined in an acid sulfate soil (ASS) wetland undergoing remediation via tidal inundation. Considerable diagenetic enrichment of reactive Fe(III) oxides (HCl- and dithionite-extractable) occurred near the soil surface (0?C0.05 m depth), where extremely large concentrations up to 3534 ??mol/g accounted for ~90% of the total Fe pool. This major source of reactive Fe exerts a substantial influence on S cycling and the formation, speciation and transformation of reduced inorganic S (RIS) in tidally inundated ASS. Under these geochemical conditions, acid volatile sulfide (AVS; up to 57 ??mol/g) and elemental sulfur (S⁰; up to 41 ??mol/g) were the dominant fractions of RIS in near surface soils. AVS?CS to pyrite?CS ratios exceeded 2.9 near the surface, indicating that abundant reactive Fe favoured the accumulation of AVS minerals and S⁰ over pyrite. This is supported by the significant correlation of poorly crystalline Fe with AVS?CS and S⁰?CS contents (r = 0.83 and r = 0.85, respectively, P < 0.01). XANES spectroscopy provided direct evidence for the presence of a greigite-like phase in AVS?CS measured by chemical extraction. While the abundant reactive Fe may limit the transformation of AVS minerals and S⁰ to pyrite during early diagenesis (~5 years), continued sulfidisation over longer time scales is likely to eventually lead to enhanced sequestration of S within pyrite (with a predicted 8% pyrite by mass). These findings provide an important understanding of sulfidisation processes occurring in reactive Fe-enriched, tidally inundated ASS landscapes.     

Pyrite oxidation by thermophilic archaebacteria

Three species of thermophilic archaebacteria of the genera Sulfolobus (Sulfolobus acidocaldarius and S. solfataricus) and Acidianus (Acidianus brierleyi) were tested for their ability to oxidize pyrite and to grow autotrophically on pyrite, to explore their potential for use in coal desulfurization. Only A. brierleyi was able to oxidize and grow autotrophically on pyrite. Jarosite was formed during the pyrite oxidation, resulting in the precipitation of sulfate and iron. The medium composition affected the extent of jarosite formation.     

Involvement of Sulfur- and Iron-Transforming Bacteria in Heaving of House Foundations

About 1,000 houses built on excavated nonweathered mudstone sediments, originally deposited in the Neogene, have been damaged by microbially induced heaving of foundations. The maximal height of the heaving was 48 cm. The presence of sulfate-reducing, sulfur-oxidizing, and acidophilic iron-oxidizing bacteria in the mudstone indicated that the joint activity of these three types of bacteria could account for the heaving. A hypothesis is presented in which, first, the temperature of the newly exposed mudstone sediments increased above 25 °C, which stimulated the sulfate-reducing bacteria in the mudstone to actively reduce sulfate to hydrogen sulfide. The mudstone sediments under the houses gradually dried, and became permeable to air. Consequently, sulfur-oxidizing bacteria oxidized the hydrogen sulfide to sulfuric acid and the environmental pH decreased to approximately 3. Next, the acidophilic iron-oxidizing bacteria actively oxidized the sulfur in pyrite to produce much more acid. The resulting sulfuric acid reacted with calcium carbonate and with ferric and potassium ions to produce gypsum and jarosite, respectively. A combination of the increased volume of gypsum and jarosite crystals and the production of CO 2 as a by-product of their formation made the mudstone sediments bulky. The end result was widespread heaving.     

Pyrite oxidation by thermophilic archaebacteria.

Three species of thermophilic archaebacteria of the genera Sulfolobus (Sulfolobus acidocaldarius and S. solfataricus) and Acidianus (Acidianus brierleyi) were tested for their ability to oxidize pyrite and to grow autotrophically on pyrite, to explore their potential for use in coal desulfurization. Only A. brierleyi was able to oxidize and grow autotrophically on pyrite. Jarosite was formed during the pyrite oxidation, resulting in the precipitation of sulfate and iron. The medium composition affected the extent of jarosite formation.     

Matrix composition and community structure analysis of a novel bacterial pyrite leaching community

Here we describe a novel bacterial community that is embedded in a matrix of carbohydrates and bio/geochemical products of pyrite (FeS₂) oxidation. This community grows in stalactite-like structures – snottites – on the ceiling of an abandoned pyrite mine at pH values of 2.2–2.6. The aqueous phase in the matrix contains 200 mM of sulfate and total iron concentrations of 60 mM. Micro-X-ray diffraction analysis showed that jarosite [(K,Na,H₃O)Fe₃(SO₄)₂(OH)₆] is the major mineral embedded in the snottites. X-ray absorption near-edge structure experiments revealed three different sulfur species. The major signal can be ascribed to sulfate, and the other two features may correspond to thiols and sulfoxides. Arabinose was detected as the major sugar component in the extracellular polymeric substance. Via restriction fragment length polymorphism analysis, a community was found that mainly consists of iron oxidizing Leptospirillum and Ferrovum species but also of bacteria that could be involved in dissimilatory sulfate and dissimilatory iron reduction. Each snottite can be regarded as a complex, self-contained consortium of bacterial species fuelled by the decomposition of pyrite.     

Isolation and partial characterization of forest floor and soil organic sulfur

The formation of organic sulfur from inorganic sulfate was investigated in hardwood forest floor and mineral horizons. All samples converted sulfate-sulfur into a non-salt extractable form which was recoverable only under conditions which release organic matter. This conversion was inhibited by azide, and depending upon the horizon, by erythromycin, candicidin, chloramphenicol and tetracycline. The form of sulfur generated in the 02 forest floor layer and in Al-horizon soil was characterized after isolation by pyrophosphate extraction at pH 8. The organosulfur extracts exhibited an average C:N:S ratio of 103:6:1. The ester sulfate content of the 02 extract was 61% by hydriodic acid (HI) reduction and 62% by hydrolysis in 3N HCl at 121 °C. However, compared to hydrolysis, reduction yielded lower estimates of ester sulfate for two of the three soil extracts analyzed. In view of the electrophoretic heterogeneity of all extracts, it is suggested that some may contain stable ester linkages that hydrolyze only after prolonged treatment and that the standard procedure for HI-reduction may provide conditions of temperature and contact time with the acid which are insufficient for the release of sulfate from these esters.Author to whom reprint requests should be addressed     

Karst development and sulfur deposit formation in the Ordos Basin: The role of bacterial sulfate reduction

Bacterial sulfate reduction is significant for the karst development and pyrite formation within the Ordovician weathering crust in the Ordos Basin of China. Bacterial communities were studied to determine their potential geomicrobiological functioning by constructing 16S rRNA clone library for in situ samples. The results showed that 147 positive clones sequenced were divided into 23 operational taxonomic units (OTUs), 8 OTUs accouting for 80% of all the selected clones belonged to the genus Desulfosporosinus. Bacterial sulfate reduction has been demonstrated to take place in the Ordovician by the classical hydrogeological information together with the stable sulfur isotope analysis from both the pyrite in the weathering crust and the products of the laboratory experiments on the dissolution of sulfate rock. The H₂S produced by bacterial sulfate reduction combined with iron to form pyrite, resulting in the development of hypogenic karst in the weathering crust. This process provided a reasonable interpretation for karst development in the vicinity of sulfur deposits in the Ordos Basin.