不同水平硝态氮对蚕豆根系质子释放量的影响

为了解豆科植物在加速土壤酸化中的作用及其机制,通过水培试验和恒pH自动电位滴定法研究了4个硝态氮供应水平对蚕豆根系质子释放量和介质pH的影响,分析了蚕豆根系释放质子的机制。结果表明,当不供应外源硝态氮时,蚕豆根系释放的质子数量最多,以干根计算培养10次的累积释放量可达37.5mmol·g-1;此条件下质子释放导致培养液pH下降幅度最大,可达1.93。随着外源硝态氮供应量的增加,蚕豆根系释放的质子数量和介质pH的下降幅度均减小。当培养液NO3-浓度为1.0mmol·L-1时,培养试验前期根系有少量质子释放,培养试验后期有少量OH-释放。研究表明,蚕豆生长介质中的质子主要来源于蚕豆根系质子的直接释放,有机酸对介质质子的贡献可以忽略。蚕豆根系对阴、阳离子的不平衡吸收是根系释放质子的主要原因,添加硝态氮可以减少蚕豆根系质子释放量。     

重庆茶园土壤酸化及肥力特征的研究

本文主要运用数理统计的方法对重庆茶园土壤的酸化特性和肥力特征作了一系列的相关分析,结果表明茶园土壤在不同pH值区段内的化学性质随pH值的变化差异明显,特别是当土壤pH值处于4.55.0区段时,对于酸化过程的抑制能力明显减弱,其盐基离子的脱除速度也显著增加,交换性阳离子中致酸离子比例增大,而当土壤pH值处于5.0以上区段时,对于酸化过程的抑制能力则明显增强,盐基脱除速度也迅速下降,交换性阳离子中致酸离子比例下降。随着土壤有机质含量的增加,其致酸离子的含量也在增加,这也就促进了土壤盐基的迅速脱除,导致土壤进一步酸化。另外,茶园土壤中的肥力特征在各pH区段也表现出较为明显的差异.在整个茶园土壤中,磷、钾、锌等植物生长所必需的元素均有不同程度的缺失,而以磷、钾的缺失尤其严重,这充分说明土壤酸化程度加剧对茶树生长十分不利。     

水稻根尖细胞原生质膜表面电势对不同氮形态、 铝和pH的响应

相对于NO_3~--N,NH_4~+-N可以缓解植物铝毒害,但其机制还不清楚。铝在细胞膜表面的吸附量受细胞膜表面电势影响,直接影响到铝毒害。本文采用酶解法提取水稻根尖原生质体,研究了原生质膜表面zeta(ξ)电势对NH_4~+N、NO_3~--N、铝和pH的响应。结果表明,不管是否加铝,NH_4~+-N和NO_3~--N本身并不显著影响原生质膜表面ξ电势,但是加铝和降低pH均可以去极化原生质膜表面ξ电势。水稻吸收NH_4~+-N一般降低生长介质pH,吸收NO_3~--N升高生长介质pH。因此,NH_4~+-N缓解水稻铝毒的原因,不是因为NH_4~+-N本身去极化了细胞膜表面电势,而是因为水稻吸收NH_4~+-N降低了介质pH,去极化了细胞膜表面电势,从而可能降低了铝在水稻根尖表面的吸附。     

硅对大麦铝毒的消除和缓解作用研究

在温室和实验室进行了施硅对消除或缓解大麦酸害铝毒的土培和溶液培养试验。结果表明,施硅后大麦幼苗的地上部茎、叶和地下部根的生物量均比不施硅明显增加。施硅能有效地促使植株吸收的铝在根部积累,抑制铝向地上部分运转;施硅还能调节根吸收的磷向地上部分运移,以减轻因伴随铝毒而产生的缺磷症状。施硅消除或缓解酸害铝毒的可能机理是:铝与硅形成无毒的铝硅酸复合离子(HAS),降低活性铝的浓度,及硅能调节大麦幼苗地上部和根内铝和磷的再分配。     

武陵山地植烟土壤酸度特征及影响因素——以湖南省湘西自治州为例

为了解多年种植烤烟的山地土壤酸度特征,研究了湘西自治州的土壤酸度指标特征及其关系以及植烟年限和土壤类型、有机质、黏粒对土壤酸度的影响。结果表明:(1)植烟年限对土壤酸度的影响大于土壤类型;随植烟年限增加,土壤pH下降,潜性酸度增加,黄棕壤土的交换性盐基、阳离子交换量和盐基饱和度下降。(2)土壤pH与交换性酸为幂函数关系,交换性铝是土壤交换性酸的主体,土壤交换性酸强度随交换性铝及其相对比例的增加而增加。(3)土壤pH与交换性盐基、阳离子交换量、盐基饱和度为二次曲线关系,当pH6时,随土壤pH增加,交换性盐基和阳离子交换量下降,盐基饱和度增加;当pH6时,随土壤pH增加,交换性盐基和阳离子交换量增加,盐基饱和度变幅小。(4)土壤交换性盐基离子主要是交换性钙,其次是交换性镁;对土壤pH影响较大的盐基离子是交换性钙。(5)有机质和黏粒主要影响土壤pH、阳离子交换量、交换性盐基和交换性钙。     

荞麦对酸铝胁迫生理响应的研究

铝毒害是限制酸性土壤中植物生长的重要因素,以荞麦(FagopyrumesculentumMoench.)为实验材料,在沙培条件下,用不同浓度(0,10,100,1000mg/L)、不同pH(3,4,5)的铝溶液处理,在出苗后的第14d和28d测试与铝胁迫有直接关系的5个生理指标。结果表明,溶液的铝浓度和pH的变化对荞麦生理都有明显的影响,最低浓度的铝处理10mg/L在不同pH下已经影响了荞麦的正常生长,和对照相比根系活力(RA)下降、根质膜透性(MP)增大、叶片内丙二醛(MDA)和游离脯氨酸(Pro)的含量以及过氧化物酶(POD)的活性升高,并且随着铝处理浓度的升高,荞麦体内各生理指标和对照差异性加大;同一铝浓度下pH5和pH3相比,MP降低、RA增强、叶片内MDA和Pro的含量以及POD的活性有所下降。铝胁迫下荞麦体内各生理指标的变化有显著的相关性。随着荞麦的生长,铝毒害有所缓解。     

流动电位法研究高岭石胶体对包铝石英砂zeta电位的影响

为探讨采用流动电位法表征带电颗粒间相互作用的可行性,采用自制的流动电位测量装置测定了高岭石胶体流经包铝石英砂时zeta电位的变化(Δζ),研究高岭石与包铝石英砂之间的作用程度,考察了包铝程度、介质离子强度和离子种类对带电颗粒之间相互作用的影响。结果表明,可采用流动电位法表征不同尺寸的异电荷颗粒间的相互作用。随着石英砂表面包铝程度的增加和介质离子强度的降低,包铝石英砂的Δζ增加,说明其与高岭石之间的作用程度增加。含低价态离子的溶液中高岭石胶体与包铝石英砂的作用程度大于其在含有高价离子的溶液中。采用经典的DLVO理论计算得到的高岭石胶体与包铝石英砂间的作用能可以很好地解释高岭石对包铝石英砂表面电化学性质的影响,两种异电荷颗粒间的静电引力大小是决定高岭石与包铝石英砂间作用程度的关键因素。在静电力的作用下,高岭石通过电荷屏蔽作用和双电层重叠作用改变包铝石英砂的zeta电位。高岭石与包铝石英砂间的静电引力越大,高岭石对包铝石英砂表面电化学性质的影响越大。     

施用稻草对酸性红壤活性铝的动态影响

酸性红壤区土壤活性铝含量的变化,对作物生长有重要影响。通过室内培养试验研究了施用不等量稻草对酸性红壤水溶性有机碳、pH值和土壤交换性铝和有机络合态铝的动态变化。结果表明,土壤水溶性有机碳在第一天达到最大值,之后开始下降直至趋于平衡。土壤pH值在前10天内快速提高,添加的稻草量越大,提高的幅度也越大,之后缓慢下降至第30天渐趋平衡;土壤交换性铝则是先降低,10天后逐渐增加至稳定状态。有机络合态铝在可溶性有机碳和有机酸等小分子化合物的联合作用下,先增加而后降低。在稻草分解的前10天,土壤水溶性碳、小分子化合物和土壤pH值对铝形态的影响均较大,而到实验后期,土壤pH值发挥着主导作用。     

铜、铅单一及其复合污染对鱼腥草吸收累积铜和铅的影响

采用溶液培养法研究铜、铅在单一及其复合污染条件下对鱼腥草吸收累积铜和铅的影响。试验结果表明,随着溶液中离子浓度的增加,鱼腥草对铜和铅的吸收累积量增加。鱼腥草累积铜的趋势以二次曲线拟合最好,累积铅的趋势以对数曲线拟合最好。在一定浓度范围内地下部对铜的富集系数随溶液中铜离子浓度的增加变小,地上部对铜的富集系数随溶液中铜离子浓度的增加变大;各部位对铅的富集系数则随溶液中铅离子浓度的增加变小。铜、铅复合污染影响鱼腥草对铜和铅的吸收累积,通过多元回归分析结果表明,铜、铅在鱼腥草植株内的累积主要表现为协同作用。     

枸杞幼苗对钒(Ⅴ)的吸收动力学特性研究

采用水培实验,研究了溶液酸度、钒(Ⅴ)离子浓度、吸收时间和钒-镉(V-Cd)复合胁迫下枸杞幼苗对V的吸收动力学特性。结果表明,pH是影响枸杞幼苗对V吸收的重要指标,随着溶液pH值增大,枸杞幼苗对V的吸收速率增大;随着吸收时间的增加,枸杞幼苗对V的吸收速率先增大后减小。在pH值为8.5的溶液中培养24 h,枸杞幼苗对V的吸收达到最大值,用Lineweaver-Burk作图法求解得最大吸收速率(Vmax)为1.67×103ng g-1h-1。与单独V处理比较,在V-Cd复合胁迫中,随着Cd(Ⅱ)浓度由0增加到30 mg L-1,枸杞幼苗的Vmax由151.5 ng g-1h-1增加至1.58×103ng g-1h-1,表明Cd(Ⅱ)浓度的增加会刺激枸杞幼苗对V的吸收。     

Tea plant (Camellia sinensis L.) roots secrete oxalic acid and caffeine into medium containing aluminum

We examined the response of the tea plant (Camellia sinensis L.) to aluminum (Al) exposure under sterile conditions, focusing specifically on the secretion of low molecular mass organic compounds from roots. After germination in agar medium, tea seedlings together with medium were placed on agar containing 0.4?mM Al with 0.2% hematoxyline (hematoxylin-Al medium). The purple color of the hematoxylin-Al medium was observed to fade gradually, until none of the color remained 6 days later. The tea seedlings were then treated with simple calcium solution (0.2?mM, at pH 4.2) containing AlCl₃, which ranged in concentration from 0 to 0.8?mM, for 24?hrs. The amount of oxalate secreted into the medium increased as the external Al concentration increased, while the concentrations of malate and citrate in the medium remained unchanged. Oxalate secretion started within 30?min after Al exposure and increased linearly thereafter. The findings demonstrated that oxalate was a key compound in the Al-tolerance mechanism employed by the tea plant, which detoxifies Al³⁺ externally in the rhizosphere. In addition to oxalate, caffeine was also secreted by tea roots in response to Al exposure. It is possible that caffeine excretion from the roots of tea plants may stimulate root growth through the inhibition of callose deposition in root tips.     

四环素类抗生素在土壤和堆肥中的吸附和降解

Two agricultural soils were collected from Dahu and Pinchen counties and swine manure compost (SMC) from Ping-tung County in Taiwan, China to investigate the sorption and dissipation of three tetracyclines (TCs), i.e., oxytetracycline (OTC), tetracycline (TC) and chlortetracycline (CTC), in compost, soils and soil/compost mixtures with different organic carbon (OC) contents. There were seven treatments in total. TCs were most strongly adsorbed to SMC in all treatments due to the high OC content. When SMC was present in the soils, the sorption of TCs was significantly enhanced, which might be attributed to the increased OC content and CEC. The adsorption of TCs showed non-linear adsorption isotherms and fitted well to the Freundlich model. After 49 d of incubation at 25 ℃ in soils and soil/compost mixtures in the dark, TCs elapsed in all substrates, with the time required for 50% degradation (DT₅₀) between 20 and 41 d, and the time for 90% degradation (DT₉₀) between 68 and 137 d. Soil amended with compost enhanced the stability of TCs and reduced their mobility. The dissipation of TCs in a soil environment was slow, indicating that these compounds might be persistent in soil.     

茶多酚和铜对可变电荷土壤钙镁释放的影响

通过批平衡试验,研究茶多酚、铜和体系pH对可变电荷土壤释放钙镁离子的影响。研究发现,铜离子初始浓度为2.0mmol/L,最终体系pH为5.0时,随着茶多酚添加量的增加,可变电荷土壤表面的负电荷增加,土壤表面释放的钙镁离子量减少。茶多酚初始添加量为20 g/kg,最终体系pH为5.0时,随着铜离子初始浓度的升高,可变电荷土壤对铜离子的吸附量增加,铜离子通过与钙镁离子发生离子交换,形成对吸附位点的竞争,从而增加钙镁离子的释放。茶多酚初始添加量为20 g/kg,铜离子浓度为2.0 mmol/L,随着pH的升高,可变电荷土壤钙镁离子释放量下降。在相同pH条件下,茶多酚可以通过自身的吸附增加可变电荷土壤表面负电荷,减少可变电荷土壤钙镁离子的释放量。研究结果可为茶园土壤酸化和污染控制提供参考。     

Aluminum-Enhanced Proton Release Associated with Plasma Membrane H+-Adenosine Triphosphatase Activity and Excess Cation Uptake in Tea (Camellia sinensis) Plant Roots

Cultivated tea (Camellia sinensis) plants acidify the rhizosphere, and Aluminum (Al) toxicity is recognized as a major limiting factor for plant growth in acidic soils. However, the mechanisms responsible for rhizosphere acidification associated with Al have not been fully elucidated. The present study examined the effect of Al on root-induced rhizosphere acidification, plasma membrane H⁺-adenosine triphosphatase (H⁺-ATPase) activity, and cation-anion balance in tea plant roots. The exudation of H⁺ from tea plant roots with or without Al treatment was visualized using an agar sheet with bromocresol purple. The H⁺-ATPase activity of plasma membranes isolated from the roots was measured after hydrolysis using the two-phase partition system. The Al treatment strongly enhanced the exudation of H⁺, and the acidification of tea plant roots by Al was closely associated with plasma membrane H⁺-ATPase activity. The root plasma membrane H⁺-ATPase activity increased with Al concentration. The Al content, amount of protons released, and H⁺-ATPase activity were significantly higher in roots treated with Al than in those untreated. The results of the cation-anion balance in roots showed an excess of cations relative to anions, with the amount of excess cation uptake increasing with increasing Al concentrations. These suggest that Al-enhanced proton release is associated with plasma membrane H⁺-ATPase activity and excess cation uptake. Findings of this study would provide insights into the contributing factors of soil acidification in tea plantations.     

茶园土壤pH变化对土壤中铝特性的影响

土壤中铝的毒性强弱取决于铝的形态。为了解茶园土壤中铝的特性,以江苏省7个长期定位观测茶园为研究对象,采用化学连续提取法测定不同条件下土样中不同形态的铝含量,研究茶园土壤pH升高或降低过程中铝的形态转化及其影响因素。结果表明,茶园土壤在酸化过程中活性铝溶出明显增强,不同形态的铝含量有明显差异,依次为腐殖酸铝(Alh)铝的水合化物和氢氧化物(Aloh)交换态铝(Alex)有机态铝(Alo)水溶态铝(Alw)无机吸附态铝(Alino);土壤pH、有机质和酸容量是影响铝形态的重要因素;茶园土壤酸化过程中铝的水合化物和氢氧化物、无机吸附态铝以及水溶态铝会转化为交换态铝。土壤pH升高,交换态铝转化成羟基铝;有机结合态铝会影响其他铝形态的转化,腐殖酸铝在土壤pH升高时转化为铝的水合化物和氢氧化物。     

模拟酸雨和外源铝对茶树铝及一些营养元素吸收积累的影响

采用盆栽方法,研究了模拟酸雨和外源铝对茶树铝及一些营养元素吸收积累的影响,以期为酸沉降区茶园管理提供资料。结果表明,随着外源铝浓度的增加,茶树根、茎和叶中铝含量增加,在适度浓度外源铝处理下,模拟酸雨促进茶树根、茎和叶对铝的吸收与积累,高酸高铝则抑制茶树各器官中铝的积累。外源铝促进茶树根、茎和叶对磷、铜和铁的吸收与积累,促进茶树茎和叶对钾的吸收与积累,对茶树根中钾含量没有明显的影响,外源铝抑制茶树根对钙、镁和锌的吸收与积累,但不影响它们在茶树中的运输,茎和叶中含量增加。模拟酸雨对茶树根和茎中磷含量没有明显影响,pH4.5的模拟酸雨有利于茶叶磷的积累,模拟酸雨对茶树根、茎和叶中钾、钙、镁、铜和锌含量没有明显的影响。无外源铝处理下,模拟酸雨降低茶树根系中铁的含量,对茎和叶中铁含量没有明显影响,外源铝处理下,模拟酸雨明显降低茶树根、茎和叶中铁的含量,并且外源铝处理浓度越高,模拟酸雨对根、茎和叶中铁含量的降低幅度越大。     

Alberta油砂地区在两种水文流域森林土壤酸化敏感性研究

Input of large amounts of N and S compounds into forest ecosystems through atmospheric deposition is a significant risk for soil acidification in the oil sands region of Alberta. We evaluated the sensitivity of forest soils to acidification in two watersheds （Lake 287 and Lake 185） with contrasting hydrological regimes as a part of a larger project assessing the role of N and S cycling in soil acidification in forest ecosystems. Fifty six forest soil samples were collected from the two watersheds by horizon from 10 monitoring plots dominated by either jack pine （Pinus banksiana） or aspen （Populus tremuloides）. Soils in the two watersheds were extremely to moderately acidic with pH （CaCl2） ranging from 2.83 to 4.91. Soil acid-base chemistry variables such as pH, base saturation, Al saturation, and acid-buffering capacity measured using the acetic acid equilibrium procedure indicated that soils in Lake 287 were more acidified than those in Lake 185. Acid-buffering capacity decreased in the order of forest floor 〉 subsurface mineral soil 〉 surface mineral soil. The most dramatic differences in percent Ca and Al saturations between the two watersheds were found in the surface mineral soil horizon. Percent Ca and Al saturation in the surface mineral soil in Lake 287 were 15% and 70%, respectively; the percent Ca saturation value fell within a critical range proposed in the literature that indicates soil acidification. Our results suggest that the soils in the two watersheds have low acid buffering capacity and would be sensitive to increased acidic deposition in the region.     

Effect of Glomus etunicatum inoculation on aluminum,phosphorus, calcium,and magnesium uptake of two barley genotypes with different aluminum tolerance

Abstract

This study was conducted to evaluate the effect of vesicular‐arbuscular mycorrhizal (VAM) fungus Glomus etunicatum on growth, absorption, and distribution of calcium (Ca), magnesium (Mg), phosphorus (P), and aluminum (Al) in one Al‐tolerant and one Al‐sensitive barley cultivar. The plants were grown in sand daily irrigated with nutrient solution containing 0 or 600 μM Al at pH 4.8. Significant interaction (P=0.05) among variety, mycorrhiza, and aluminum (VxMxAl) were noted for both shoot and root dry matter (DM); shoot concentration and content of Al, P, Ca, and Mg; root concentration of Al, P, and Mg; and root content of Al, P, Ca, and Mg. With VAM inoculation: i) root colonization degree was about 50% in all treatment, ii) shoot DM yield increased between 30 and 70%, iii) Al concentration and content decrease down to a half both in shoots and roots of sensitive barley, iv) Ca concentration in shoots of sensitive barley showed a high increase at 600 μM Al, and v) P concentration and content in shoots of both varieties increased significantly.     

Effects of long‐term applications of various nitrogen sources on chemical soil properties and composition of bromegrass hay

Effects of 15 annual applications (from 1979 to 1993) of ammonium nitrate (AN), urea, ammonium sulfate (AS), and calcium nitrate (CN) applied at 168 and 336 kg N ha^‐1 to bromegrass (Bromus inermis Leyss.) on soil acidification, and concentration of aluminum (Al), iron (Fe), manganese (Mn), zinc (Zn), and copper (Cu) in soil and in hay were investigated in a field experiment on a thin Black Chemozemic (Typic Boroll) soil in Alberta, Canada. Soil was acidified and the concentration of extractable Al, Fe, and Mn was increased by nitrogen (N) application, but the magnitude varied with N source. Soil acidification was greatest with AS, followed by AN and urea, with no effect of CN. At 336 kg N ha^‐1 rate, soil was acidified to a depth of 10, 15 and 30 cm with urea, AN AS, respectively. Soil acidification was also greater at 336 kg than 168 kg N ha^‐1. The CaCl₂‐extractable Al and Fe in the 0–15 cm layer increased with N application, which closely followed the decrease in soil pH from various N sources. Extractable Al and Fe concentration in the 15–30 cm layer increased in response to reduction in soil pH by AS only, and there was no change in the extractable Al and Fe below the 30‐cm depth by any form of N. The DTPA‐extractable Mn in soil generally changed in response to N application. There was no effect of N source on the DTPA‐extractable Zn and Cu in soil. When soil pH had been lowered from N application, the concentration of Al in hay decreased while Zn concentration increased. The Mn concentration in forage increased markedly in response to reduced soil pH from application of AN, urea and AS. There was no effect of N fertilization on the Cu and Fe concentration in hay. In conclusion, the magnitude of soil acidification, changes in the Al, Fe, and Mn concentrations in soil and changes in the Al, Zn, and Mn concentrations in bromegrass hay varied with N source. The results suggest the need for periodic monitoring of soil pH and consideration of liming costs in the economics of various N fertilizers.     

Effect of nodulation with Bradyrhizobium japonicum and Shinorhizobium fredii on xylem sap composition of Peking (Glycine max L. Merr )

Five barley cultivars were grown together in complete, low-P·low-pH and high-Al medium containing only NO₃, only NH₄ or both NO₃ and NH₄ as N sources, respectively using an automatic control system of pH for water culture, and the relationship between the differential Al tolerance and the plant-induced pH change of medium among the barley cultivars was investigated.

The pH of the medium containing only NO₃ as N source tended to increase, whereas the pH of the other media containing only NH₄ or both NO₃ and NH₄ as N sources tended to decrease, but the fluctuations of the medium pH could be maintained within the value of 0.2 pH in the complete medium and within the value of 0.1 pH in the high-Al medium.

Barley cultivars still differed in their Al tolerance in the medium which was continuously stirred and circulated at a constant pH. The pattern of Al tolerance was not affected by the N sources in the medium. The plant-induced pH change of medium for each cultivar was influenced by the N sources in the medium, and was not correlated positively with Al tolerance. The contents of Al and Ca or other nutrient cations in roots were positively correlated with Al tolerance and positive correlations were recognized also between the contents of Al and Ca or some other nutrient cations in the roots.

In conclusion, the following mechanisms are proposed. Al tolerant barley cultivars exclude Al actively outside the plasmalemma of the root cells, and the excluded Al may polymerize and or react with P to form Al precipitates. Consequently, in the Al tolerant barley cultivars the Al content may be low in the root protoplasts, high in the whole root tissues and the contents of Ca or other nutrients may be high in the roots. The plant-induced pH change of medium is not considered to be the cause of the differential Al tolerance among barley cultivars.