A Preliminary Study on Physiological and Molecular Effects of Iron Deficiency in Fuji/Chistock 1

In order to get experimental data on apple rootstock with iron-efficient genotypes capable of improving scion resistance to iron deficiency, this experiment was conducted on the physiological and molecular characteristics of Fuji/ Chistock 1 (F/C) under different iron conditions and compared it to Fuji/ M. Baccata (F/B). F/C was less sensitive to iron deficiency than F/B. F/B showed chlorosis after 25 days under iron-deficient conditions, but F/C showed no phenotypic changes, even after 40 days. The shoot and leaf area growth of F/C were respectively 5cm and 1000 mm² higher than those of F/B, regardless of the iron-deficient or iron-efficient conditions. The young leaf chlorophyll and active iron of F/C were 5 SPAD and 5 mg kg^?1 higher than those of F/B, either in iron-deficient or iron-efficient conditions. The expression of YSL5 and CS1 showed the same pattern. The enhancement expression of iron transport genes may be one explanation for these findings.     

运用简单线性水库模型计算Pothwar黄土平原（巴基斯坦）磷灰石损失情况

Apatite is the dominant phosphorus （P） mineral in early stages of soil development, and its redistribution as labile forms under pedogenesis controls terrestrial bioavailability. Quantitative distribution of labile forms of P and apatite-P was examined in Pothwar Loess Plain, Pakistan where the degree of pedogenesis varied with relief. Four soil types, Typic Ustorthents （Rajar）, Typic Calciustepts （Missa）, Udic Calciustepts （Basal）, and Udic Haplustalfs （Guliana）, were sampled from three replicated locations at genetic horizon level. With the exception of total P value at surface, the mean total and apatite-P decreased towards the surface in Udic Haplustalfs and Udic Calciustepts where dicalcium and octacalcium phosphate increased toward surface. Iron （oxides and oxyhydroxides） adsorbed and occluded P forms were also in greater quantities in Udic Haplustalfs and increased toward the surface, whereas they were lowest and uniform in the Typic Ustorthents. Aluminum- and organic P correlated with soil organic matter. Apatite-P decreased exponentially with an increase in the sum of iron adsorbed and occluded P fractions, and fitted the equation M（x） =M0[1 - exp（-wx）] with r^2=0.996, where M（x） is the mean apatite-P concentration in solum, M0 is the apatite-P content in the loess sediments, x is the cumulative iron adsorbed and occluded P, and w is an empirical factor indicating the change rate of apatite-P in the loess. From the calculated apatite-P of 740 mg kg^-1 at the time of deposition, mean apatite-P loss was 60% in Udic Haplustalfs, 33% in Udic Calciustepts, 23% in Typic Calciustepts, and 8% in Typic Ustorthents. The transformation of soil P to labile forms was faster and deeper in level or slight depressions followed by gently sloping areas in wide plains, and was the least in the gullied land.     

Effect of P fertilizer reduction regime on soil Olsen-P, root Fe-plaque P, and rice P uptake in rice-wheat rotation paddy fields

In agricultural systems, it is vital to use limited yet optimal phosphorus(P) resources, because excessive P fertilizer application leads to the accumulation of P in soil, increasing the risk of environmental pollution and causing the waste and exhaustion of P resources. In a rice-wheat rotation system, omitting P fertilizer application in the rice-growing season is a good alternative;however, how this P fertilization reduction influences changes in P in the soil-root-aboveground system is unclear. In this study, after a seven-year rice-wheat rotation at the Yixing(YX) and Changshu(CS) sampling sites, China, compared with P fertilization in rice-and wheat-growing seasons(PR+W), reduced P fertilization(no P fertilizer application in either season, P0;P fertilization only in wheat-growing seasons, PW;and P fertilization only in rice-growing seasons, PR) did not result in substantial variation in crop biomass. The PW treatment did not reduce crop total P, root iron(Fe)-plaque P, and soil Olsen-P at three stages of rice growth(seedling, booting, and harvesting stages) at the YX and CS sites. In contrast, concentrations of soil Olsen-P, aboveground crop total P, and root Fe-plaque P decreased in the P0 treatment by 45.8%–81.0%,24.6%–30.9%, and 45.6%–73.4%, respectively. In addition, a significant negative correlation was observed between the root Fe-plaque P and crop biomass at the two sites. Significant positive correlations were also observed between root Fe-plaque P and root total P, crop total P, and soil Olsen-P. In addition, the results of a redundancy analysis revealed that soil alkaline phosphatase(ALP) played a major role in the supply of P in soil, and was closely associated with root Fe-plaque P. The results of this study will enhance the understanding of the changes in P in the soil-root-aboveground system, particularly under P fertilizer reduction regimes.     

波兰喀尔巴阡山麓漂白淋溶土中铁锰结核的分布、形态和化学组成研究

Iron and manganese oxides are common components of soils. They frequently occur in nodules constituting important soil sorbents and play a crucial role in a number of chemical reactions in the soil environment. In addition, the oxides are very sensitive to environmental changes (moisture, pH, Eh) constituting important indicators of soil-forming processes and water movement in the landscape. The objectives of the study were: i) to examine the distribution and size of Fe-Mn nodules in Albeluvisols containing a fragipan horizon; ii) to determine the morphology and chemical composition of the nodules, and iii) to estimate the effect of the fragipan horizon on water movement within the soil profile. An investigation was carried out on five soil profiles containing a fragipan horizon and classified as Fragic Albeluvisols within the Carpathian Foothills in Poland. In the Albeluvisols studied, the maximum concentration of Fe-Mn nodules occurred in the horizon lying directly on the fragipan horizon. This suggests that the pan acts as a natural barrier restricting water infiltration and leads to the seasonal development of a perched water table promoting redox processes. The most common are coarse (1--0.5 mm) and medium (0.5--0.25 mm) irregular Fe-Mn nodules showing a gradual boundary and undifferentiated internal fabric. Eluvial horizons contained also larger amounts of round and dense nodules with a sharp boundary, suggesting frequent oxidation and reduction. The fragipan horizon contained mainly irregular and soft nodules, suggesting longer saturation with water during the year. Concentrations of trace elements (Cu, Zn) and P were higher within Fe-Mn nodules than in the surrounding soil materials, showing that iron and manganese oxides adsorbed and immobilised these elements.     

小金海棠类黄色条纹蛋白基因MxYSL7的克隆与表达分析

为了解铁高效基因型小金海棠抗缺铁的分子机制,对与铁运输相关的YSL基因进行了克隆与分析.分析苹果的EST库得到一个686 bp的YSL基因片段.经3′-RACE及后期拼接得到1 500 bp的该基因的3′端序列.其预测蛋白含10个跨膜区,与拟南芥AtYSL7基因同源性达71%,命名为MxYSL7.RT-PCR及Northern分析表明,小金海棠的该基因只在地上部分表达:在茎与成熟叶中,随着低铁处理时间的延长,该基因表达量减少;随着高铁处理时间的延长,该基因表达量增多.新叶中的表达趋势与茎和成熟叶中的趋势正好相反.讨论了MxYSL7在小金海棠体内铁营养代谢中的作用.认为MxYSL7可能参与了体内铁在木质部和韧皮部的运输过程,并参与铁在体内的解毒过程.     

间作条件下作物对铁的吸收利用和病害控制*

 合理间作不但有提高作物产量优势,而且铁的吸收利用效率也会提高,对病害控制有所加强。从目前对铁的研究而言,铁与作物病害的发生关系已有一些报道,但在间作条件下作物对铁的吸收利用和病害控制关系研究很少。因此,从间作条件下作物对铁的吸收利用、病害控制及铁对病害的影响3个方面进行文献综述和讨论具有重要科研指导意义。     

铁在寒地早粳花药培养中的效应研究

摘要：铁是水稻花培培养基的重要成分。通过对7份寒地早粳组合F1（或品系）花药在不同Fe2+含量培养基上离体培养,发现培养基中的Fe2+的含量对诱导率、绿苗分化率影响较大。结果表明在N6培养基中将Fe2+提高到32-40mg/kg诱导率最大,高于N6培养基（Fe2+含量为5.6mg/kg）1.4倍以上。在此以内随着Fe2+含量的增加诱导率增加,大于此含量诱导率降低,呈单峰曲线分布。分化培养基中Fe2+含量增加到40mg/kg分化率显著降低。但在32-40mg/kgFe2+培养基上诱导出的愈伤组织在MS培养基上的绿苗分化率差异明显,71.4%材料可使绿苗生产率提高到9.2%左右。因此适当提高诱导培养基中Fe2+含量可提高寒地早粳的花培效率。     

Effects of ferrous iron (Fe) on the germination and root elongation of paddy rice and weeds

Laboratory experiments were conducted to analyze the iron (Fe) tolerance of paddy weeds and rice varieties (Oryza sativa) for germination and root elongation. Under a waterlogged soil condition, the Fe(II) content in a soil solution increased with an increase in the ratio of rice straw to the soil. In the presence of 0.9% (w/w) straw to soil, which corresponds approximately to 8 t of straw applied to an area of 1 ha × 10 cm depth in the field, ～80 mg L^?1 of Fe(II) was produced in the soil solution. Based on this result, the seeds of rice and the weeds were incubated in a solution with <100 mg L^?1 of Fe(II). The presence of 100 mg L^?1 of Fe(II) suppressed the germination of Echinochloa crus‐galli var. crus‐galli, Cyperus serotinus, Cyperus difformis, and Monochoria korsakowii. However, it had no effect on the germination of Echinochloa oryzicola, Schoenoplectus juncoides (= Scirpus juncoides var. ohwianus), and Monochoria vaginalis. This level of Fe tolerance was the same as that of rice. These findings suggest that E. oryzicola, S. juncoides, and M. vaginalis can grow under more severe conditions than E. crus‐galli, C. serotinus, C. difformis, and M. korsakowii. In relation to seminal root elongation, the order of tolerance of Fe toxicity was O. sativa cv. Dunghan Shali > O. sativa cv. Hoshinoyume > E. oryzicola > M. vaginalis > S. juncoides. Thus, the results show that the tolerance of rice is greater than that of E. oryzicola, which had a comparatively strong tolerance among the weeds examined, and also that there are differences in tolerance among the rice varieties. These findings suggest that the difference in Fe tolerance is involved in weed control systems when organic materials are applied. If this difference is an important factor in the weed control system, Fe‐tolerant rice varieties, like cv. D. Shali, could facilitate weed control systems due to their higher Fe tolerance ability.     

高铁高硒日粮对鸡蛋品质的影响

用高铁高硒日粮饲喂产蛋母鸡,观察蛋品质的变化,结果表明,蛋黄重、蛋黄重／蛋重比略有下降,蛋白质／蛋重比、哈夫单位有所提高,蛋壳／蛋重比,蛋壳厚度及蛋壳密度无明显变化,提示：高铁高硒日粮不会引起蛋品质的明显下降。     

Fe(Ⅲ)-H_2O_2-甲基蓝体系催化动力学光度法测定痕量Fe(Ⅲ)

在 H2 SO4 介质中 ,痕量 Fe( )对 H2 O2 氧化甲基蓝褪色反应具有较强的催化作用 ,据此建立了一种催化动力学光度法测定痕量 Fe( )的新方法 .该方法的线性范围为 0 .0 192 - 0 .0 6 6 0μg· m L-1,检测限为 8.0 1×10 -10 g· m L-1.用于水样中痕量 Fe( )的测定 ,结果满意 .