铁在苹果树器官中的定量研究

成龄苹果树整株分析结果表明 ,果实、叶片、枝干、根系的鲜重分别占整株鲜重的 42 .0 9%、6 .33%、38.81%、12 .77% ,以果实占鲜重的比例最大 ,单株鲜重为 2 0 7.90kg ;果实、叶片、枝干、根系的干重分别占整株干重的 19.5 1%、6 .45 %、5 7.30 %、16 .75 % ,以枝干占干重的比例最大 ,单株干重 84.37kg ,单株含水量 12 3.5 5kg。铁浓度以直径 <0 .5cm的根最高 ,达 2 5 7.5 1mg/kg ,其次为叶片 ,达 2 14.0 9mg/kg ,果实中铁浓度最低 ,为 18.2 7mg/kg;单株总铁含量 4915 .78mg,叶、果、根、枝干中铁含量分别为 116 4.6 5、30 0 .72、15 0 0 .30、1949.6 0mg ,分别占单株总铁量的2 3 .70 %、6 .12 %、30 .5 2 %和 39.6 6 %。     

靠接换砧矫治枳砧甜橙缺铁黄化研究

靠接红桔、酸桔和枸头橙砧,矫治枳砧甜橙缺铁黄化有明显效果。其中,以枸头橙效果最好,以下依次为酸桔和红桔,靠接砧苗后树势逐年恢复,产量成倍增加,靠接红桔、酸桔和枸头橙分别比对照增产3.3、1.4和1.5倍;对提高果实含糖量、果汁率和降低含酸量亦有良好效果。     

山楂缺铁黄叶病及应用硝黄铁防治研究

根据调查初步总结出山楂缺铁黄叶病的发生发展规律、致病因素及其对山楂生产的危害。用新研制的高效价廉、储运方便的硝黄铁矫治,效果明显。黄化病株复绿率40%～87%,三级病株减少36%～100%,叶绿素含量提高64%～224%,喷肥区比对照区株产提高25%。同时增加了果实中糖、酸、果胶及钙、铁含量,提高了果实品质。     

铋系氧化物在光催化技术中的研究进展

总结近年铋系列半导体光催化剂的制备、种类和光催化反应机理等的研究进展,并展望了铋系列半导体光催化剂未来的发展方向.     

Predicting the degree of phosphorus saturation using the ammonium acetate–EDTA soil test

As a result of the important role played by phosphorus (P) in surface water eutrophication, the susceptibility of soils to release P requires evaluation. The degree of phosphorus saturation, assessed by oxalate extraction (DPS_ox), has been used as an indicator. However, most laboratories do not include DPS_ox in routine soil tests because of cost and time. This study evaluates the suitability of the ammonium acetate extraction in the presence of EDTA (AAEDTA), the standard soil test P (STP) in Wallonia (Southern Belgium), to predict DPS_ox; we also compared it with the Mehlich 3 extraction. Ninety‐three topsoil samples were collected in agricultural soils throughout Wallonia. Good correlations were found between the AAEDTA and the Mehlich 3 methods for P, Fe and Al (r = 0.85, 0.77 and 0.86, respectively). An exponential relationship was found between P_AAEDTA and DPS_ox. Results of principal component analysis and regression demonstrated that STP can be used to predict DPS_ox (r = 0.93) after logarithmic transformation. Soil test Al was also a good indicator of the P sorption capacity (PSC_ox) of soils (r = 0.86). Including the clay fraction in regression equations only slightly improved the prediction of PSC_ox (r = 0.90), while other readily available data (such as pH or organic carbon) did not significantly improve either DPS_ox or PSC_ox predictions.     

Contribution to the study of the podsolisation process

Abstract

Analytical data for Al and Fe extracted by different reagents is presented. It is concluded from the data that in podsolisation Al migrates mainly as inorganic gel while iron moves as organic chelated complexes.     

Evaluation of Commercial Fe(III)‐Chelates Using Different Methods

Abstract

A collaborative assay among three laboratories was made in order to compare both the ion (CEN. EN 13368‐2:2001 E. Determination of chelating agents in fertilizers by ion chromatography. Part 2: EDDHA and EDDHMA, 2001a) and the ion‐pair (Lucena, J.J.; Barak, P.; Hernandez‐Apaolaza, L. Isocratic ion‐pair high‐performance liquid chromatographic method for the determination of various iron(III) chelates. J. Chromatogr. A 1996, 727, 253–264) high performance liquid chromatography (HPLC) methods as well as the soluble and complexed Fe (CEN. EN 13366:2001 E. Treatment with a cation exchange resin for the determination of the chelated micronutrient content and of the chelated fraction of micronutrients, 2001b) methods. Fifteen and ten samples of commercial fertilizers of Fe‐EDDHA, Fe‐EDDHMA, respectively were analysed by three laboratories using these methods. No significant differences were observed between the results obtained for the Fe‐EDDHA content using the Lucena et al. or CEN method. The first method makes it possible to distinguish between the meso and DL‐racemic diasteroisomers of Fe‐o, o‐EDDHA. For the Fe‐EDDHMA formulations, the CEN method gives higher values than the ion‐pair method, since in the first one Fe‐EDDH4,6MA coelutes with FeEDDHMA. Also the CEN method does not makes it possible to distinguish between Fe‐EDDHMA and Fe‐EDDH5MA products. The variability among laboratories was larger for the CEN method than for the Lucena et al. method.     

Overload of ferric ammonium citrate triggers MAPK pathways by producing high level of reactive oxygen species and induces apoptosis of human hFOB1.19 osteoblast cells

AIM：To investigate the role of reative oxygen species (ROS) generated by iron overload in activating the mitogen-activated protein kinase (MAPK) pathways and apoptosis. METHODS：Cultured human osteoblast cell line hFOB1.19 was treated with ferric ammonium citrate (FAC) at concentrations of 0~500 μmoL/L. The proliferation of hFOB1.19 cells was analyzed by MTT assay. Apoptosis was detected by flow cytometry with Annexin V/PI staining. The expression levels of p-ERK, p-JNK and p-p38 were determined by Western blotting 24 h after treatment with FAC. RESULTS：After treated with FAC, the cell proliferation was inhibited. The early apoptosis and total cell death were significantly increased. The levels of ROS were increased to (35.73±2.52)%, (62.89±4.24)% and (76.06±3.55)% with the increasing doses of FAC treatmen,respectively. The expression levels of p-ERK, p-JNK and p-p38 were also remarkably elevated in FAC groups. CONCLUSION：Iron overload increases intracellular ROS level, thus triggering the MAPK pathways and inducing apoptosis of human hFOB1.19 osteoblast cells.     

紫色土可溶性有机碳的吸附-解吸特征

选择代表性的酸性、中性和石灰性紫色土为实验材料,采用平衡吸附和动力学吸附法研究了紫色土对可溶性有机碳（DOC）的吸附-解吸特征,分析了土壤理化性质与DOC吸附量之间的关系。结果表明,紫色土对DOC的吸附容量呈以下顺序：酸性紫色土〉中性紫色土〉石灰性紫色土。石灰性紫色土对DOC的解吸率明显高于酸性、中性紫色土,其迁移淋失问题值得重视。紫色土对DOC的吸附过程包括快速吸附和慢速吸附2个阶段,0~0.5 h内吸附速率最大,随后吸附速率逐渐减小,4~6 h内基本达到吸附平衡。土壤pH值、有机质、粘粒和活性铁铝氧化物含量是影响土壤DOC吸附量与解吸率的重要因素。通径分析表明,土壤理化性质对DOC吸附量的直接作用系数大小顺序为活性铝含量〉土壤pH值〉有机质,对DOC解吸率的直接作用系数大小顺序为活性铁含量〉粘粒〉有机质。多元线性回归模型能较好地预测土壤对DOC的吸附及解吸的变化。     

Mycorrhizal (Rhizophagus Intraradices) Symbiosis and Fe and Zn Availability in Calcareous Soil

Greenhouse experiment was conducted to assess the iron (Fe) and zinc (Zn) fractionation patterns in soils of arbuscular mycorrhizal (AM) fungus-inoculated and uninoculated maize plants fertilized with varying levels of Fe and Zn. Soil samples were collected for Fe and Zn fractions and available Fe, Zn and phosphorus (P) contents besides organic and biomass carbon (BMC), soil enzymes and glomalin. Major portion of Fe and Zn fractionations was found to occur in the residual form. Mycorrhizal symbiosis increased the organically bound forms of Fe and Zn while reducing the crystalline oxide, residual Fe and Zn fractions, indicating the transformation of unavailable forms into available forms. Soil enzymes, viz. dehydrogenase and acid phosphatase activities in M+ soils, were significantly higher than M? soil consistently. Overall, the data suggest that mycorrhizal symbiosis enhanced the availability of Fe and Zn as a result of preferential fractionation and biochemical changes that may alleviate micronutrient deficiencies in calcareous soil.

Abbreviations: AM: arbuscular mycorrhiza; Fe: Iron; Zn: Zinc; P: Phosphorous; Amox-Zn: amorphous oxide bound zinc; Cryox-Zn: crystalline oxide bound zinc; DAS: days after sowing; DTPA: diethylene Triamine Penta Acetic Acid; MnO₂-Zn: manganese oxide bound zinc; OC-Zn: organically bound zinc; WSEX: water soluble plus exchangeable zinc; MnO₂ Fe: manganese oxide bound iron; OC-Fe: Organically bound iron; WSEX Fe: water soluble plus exchangeable iron.