AlH2P3O10·2H2 O（Ⅰ）对水中Ni^2＋的吸附动力学和热力学研究

采用静态吸附法研究Al2O3-P2O5-H2O反应体系产物三聚磷酸二氢铝Ⅰ型二水物[AlH2P3O10.2H2O（Ⅰ）]吸附水中Ni2＋的动力学和热力学。考察了温度、浓度、粒径、pH和搅拌速度对吸附过程的影响,通过不同温度下的吸附等温热力学性能的变化,计算了吸附焓、吸附熵和自由能。结果表明,在试验范围内,AlH2P3O10.2H2O（Ⅰ）对Ni2＋的吸附符合Langmuir吸附等温方程式,过程受颗粒扩散控制,反应级数为1.88,298.15 K时的热力学数据为：Ea=11.561 kJ/mol,ΔH=35.75 kJ/mol,ΔS=190.58 J/（mol.K）,ΔG=-21.07 kJ/mol,吸附为自发的吸热过程,其吸附动力学总方程为：1-2/3x-（1-x）2/3=0.36r02C01.88exp（-11 561/RT）。     

矿物质调理剂中铝的稳定性及其对酸性土壤的改良作用

通过室内土壤培养试验和模拟酸雨浸泡试验,研究了3种含铝量不同的矿物质调理剂中铝的稳定性及其对酸性土壤的改良效果。该类调理剂是利用钾长石、白云石和石灰石等合理配伍后经高温焙烧而制得,呈弱碱性,富含有效钙、镁、钾、硅等营养元素。试验结果表明,施入0.5~2 g/kg调理剂培养60 d后,土壤pH由4.98升高到5.04~5.42,交换性铝含量下降37.40%~68.90%,吸附态羟基铝含量稍有增加,但毒害性铝和活性铝总量分别降低了5.37%~9.50%和4.33%~12.08%,提高土壤中交换性钙、镁、钾和有效硅的含量。同时模拟酸雨浸泡试验中铝溶出量明显降低。该类矿物质调理剂能中和土壤酸度、缓解铝毒和增加土壤养分;调理剂中铝稳定性较高,不会对土壤铝毒产生叠加效应,可安全应用于农业生产。     

甲磺酸加替沙星-Al(III)荧光体系的研究及应用

[目的]研究铝（Ⅲ）-甲磺酸加替沙星荧光体系测定微量铝（Ⅲ）方法的建立与应用。[方法]在C6H4CO2HCO2K-NaOH介质中,铝与甲磺酸加替沙星形成络合物使甲磺酸加替沙星的荧光强度（ΔF）显著增敏,由此建立了测定铝的新方法,并研究不同溶液酸度、表面活性剂、甲磺酸加替沙星用量、试剂加入顺序对该体系ΔF的影响。[结果]荧光光谱图显示,该体系的最大激发波长λex=365 nm,最大发射波长λem=470 nm。溶液的酸度对该体系的ΔF有较大影响,pH值在5.50～6.50时可使该体系的增敏作用达到最大且较稳定。加入表面活性剂对ΔF均无较明显的影响。该体系中铝的浓度在1.58×10^-8～4.24×10^-6mol/L范围内与ΔF=F-F0具有良好的线性关系,最低检出限为8.36×10^-9mol/L,回收率为99.4%～101.4%。[结论]该方法用于测定食品中微量铝的含量可获得灵敏度较高和选择性较好的结果。     

植物铝胁迫响应机制的研究进展

从铝对植物的毒害、植物耐铝（抗铝）的生理、遗传、分子生物学等多方面综述植物的耐铝机制．并探讨其研究的发展方向。     

铝胁迫对黄瓜种子发芽及抗氧化酶活性的影响

本试验以黄瓜品种津春2号为材料,研究了铝胁迫对黄瓜种子发芽及抗氧化酶活性的影响。结果表明,铝处理显著抑制了黄瓜种子萌发后根部的伸长,提高了根部抗坏血酸过氧化物酶（APX）、过氧化物酶（POD）、过氧化氢酶（CAT）和脱氢抗坏血酸还原酶（DHAR）活性。超氧化物歧化酶（SOD）在低浓度铝处理下活性升高,而在高浓度下降低。     

Land Application of Aluminum Water Treatment Residual: Aluminum Phytoavailability and Forage Yield

Negative impacts of land‐applied aluminum (Al)–rich water treatment residuals (WTRs), which have been suggested to improve soil phosphorus (P) sorption, could include excessive immobilization of plant‐available P and Al phytotoxicity. We studied the impacts of an Al‐rich WTRs on agronomic returns and plant Al concentrations in glasshouse and field studies. The glasshouse study was a 4 × 2 × 3 factorial experiment with one control in a randomized complete block design and three replicates. Four sources of P were each applied at two agronomic rate [44 kg P ha^?1, P‐based rate; and 179 kg plant‐available nitrogen (PAN) ha^?1, N‐based rate] to topsoil (0–15 cm) of a sandy, siliceous, hyperthermic Arenic Alaquods. Three WTR rates (0, 10, and 25 g kg^?1 oven‐dry‐weight basis) were further applied, whereas the control received neither P source nor WTRs. Bahiagrass (Paspalum notatum Fluggae), ryegrass (Lolium perenne L.), and a second bahiagrass crop were continuously grown in succession for 18 months. Applied WTRs increased soil Al but not plant Al concentrations (22–80 mg Al kg^?1), which fell within the normal concentration range for pasture plants. In the glasshouse, when WTRs were incorporated with the soil, bahiagrass dry matter (DM) accumulation was reduced, but ryegrass DM was not affected even at 25 g kg^?1 WTR. A 2‐year field study, with same treatments but two rates of WTRs (0 and 10 g kg^?1 WTR) surface applied to established bahiagrass on the same soil type (Spodosols) showed neither reduced yields nor increased plant Al phytoavailability in the WTR treatments. The studies show no increase in plant Al is associated with Al‐WTRs applied to reduce excess soil‐soluble P and P losses but plant DM accumulation may be reduced.     

Alfalfa Responses to Combined Use of Lime and Limiting Nutrients on an Acidic Soil

An on-farm field experiment was conducted on an acidic soil to investigate the effects of combined use of lime and deficient nutrients on herbage yield of alfalfa (Medicago sativa L.). Omitting lime and limiting nutrients led to elevated concentrations of aluminium (Al), iron (Fe), and manganese (Mn) in alfalfa leaves and stems and caused severe reductions in herbage yield of alfalfa. Combined use of lime (2 t ha^?1) and nutrients [phosphorus (P): 20 kg ha^?1, sulfur (S): 20 kg ha^?1, zinc (Zn): 4 kg ha^?1, and boron (B): 2 kg ha^?1] had the maximum increase in groundcover, root biomass, nodulation, leaf retention, leaf-to-stem ratio, herbage yield, crude protein, and nutrient composition of alfalfa. These beneficial effects were due to raised soil pH; improved calcium (Ca), P, S, Zn, and B nutrition; and reduced Al, Mn, and Fe toxicity. Aluminium and all the nutrients except copper (Cu) were more concentrated in alfalfa leaves than stems.

Aluminum concentration was about three times greater in the lower leaves than in upper leaves. Lower leaves also had much greater concentrations of Ca, Mg, K, S, Fe, Mn, Cu, and B compared with upper leaves. In contrast, P and Zn concentrations were greater in the upper leaves than in lower leaves. Results suggest that the combined use of lime and all the limiting nutrients may realize potential beneficial effects of alfalfa on acidic soils where more than one essential nutrient is deficient. This may increase growth potential, nitrogen contributions, and groundcover by alfalfa and reduce soil erosion and runoff.     

Related Characteristics and Multivariate Analyses in the Evaluation of White Oat Aluminum Tolerance

Standard white oat genotypes were subjected to different methods and aluminum (Al) levels under hydroponic conditions to verify the relationship between plantlet characteristics and their Al tolerance using multivariate analyses. A completely randomized design with three replications was used, adopting three evaluation protocols: “complete nutrient solution” with 0, 8, 16, and 32 mg L^?1 of Al supplied as aluminum sulfate [Al₂(SO₄)₃·18H₂O]; “complete nutrient solution” with 0, 8, 16 and 32 mg L^?1 of Al supplied as aluminum chloride (Al₂Cl₃?6H₂O); and the “minimum nutrient solution” with 0, 1, 3, and 5 mg L^?1 of Al supplied as Al₂Cl₃?6H₂O. The performance of white oat plantlet genotypes subjected to excess Al in hydroponic conditions is greatly associated with root length, where the nutrient solution composition and the Al sources interfere in these associations. The study based on the joint analysis of characteristics at plantlet level does not allow an efficient discrimination of Al-tolerant and Al-sensitive white oat genotypes.     

The effect of soil pH manipulation on chemical properties of an agricultural soil from northern Idaho

Abstract

Selected chemical properties of an artificially acidified agricultural soil from northern Idaho were evaluated in a laboratory study. Elemental S and Ca(OH)₂were used to manipulate the soil pH of a Latahco silt loam (fine‐silty, mixed, frigid Argiaquic Xeric Argialboll), which had an initial pH of 5.7. A 100 day incubation period resulted in a soil pH manipulation range of 3.3 to 7.0. Chemical properties evaluated included: N mineralization rate, extractable P, AI, Mn, Ca, Mg and K and CEC. N mineralization rate (assessed by anaerobic incubation) decreased with decreasing soil pH. Nitrification rate also decreased as NH₄ ⁺‐N accumulated under acid soil conditions. Sodium acetate extractable P was positively linearly correlated (R²= 0.87) with soil pH over the entire pH range evaluated. Potassium chloride extractable Al was less than 1.3 mg kg^‐1of soil at pH values higher than 4.4. Consequently, potential Al toxicity problems in these soils are minimal. Extractable Mn increased with decreasing soil pH. Soil CEC, extractable Mg, and extractable K all decreased with increasing soil pH from 3.3 to 7.0. Extractable Ca levels were largely unaffected by changing soil pH. It is likely that the availability of N and P would be the most adversely affected parameters by soil acidification