铁法预处理糖蜜酒精废液沼气发酵工艺的研究

本研究采用法法预处理糖蜜精废液，并将其进行厌氧发酵试验，试验的厌氧罐容积为１３Ｌ，预处理容积为１．３Ｌ结果表明：经铁法预处理后的糖蜜酒精度液能够稳定地用于沼气发酵，而且所产沼气的Ｈ２Ｓ含量大减少。     

H.E染色和普鲁氏染色在动物铁过负荷诊断的比较

本试验研究比较铁过负荷猪的淋巴结、脾脏、肝脏、肺脏、肾脏的H.E染色、革兰氏染色的变化。     

乳酸菌富铁的研究

为了使铁离子转化为易被动物体吸收的微量元素,以防治仔猪因缺铁而造成的贫血等病症,本研究用乳酸菌富集铁元素。首先测得乳酸菌在硫酸亚铁和有机铁2种来源的铁元素中所能正常生长的最高铁离子浓度,然后加入适宜浓度的铁离子培养乳酸菌至最高活菌数。菌液离心后冲洗3次并烘干,用原子分光光度法测定乳酸菌干细胞内铁离子的含量,比较乳酸菌对2种形态铁元素的富集能力。最后做饲养试验。结果表明:乳酸菌对有机铁的耐受质量浓度(0.5 g/L)比硫酸亚铁(0.1 g/L)高;乳酸菌对有机铁的富集能力(1.590 mg/g)比硫酸亚铁(0.024mg/g)强。含有机铁的乳酸菌制剂对降低断奶仔猪死亡率有显著效果。     

苜蓿草粉比例对豁鹅蛋黄铁锌含量的影响

本试验采用3×3因子设计,将日粮苜蓿草粉比例设为10%、20%、30%三个水平、蛋白质设为15.83%、14.01%、12.74%三个水平。选用180只12月龄健康产蛋豁鹅,随机分为9组,每组20只,试验期20d。研究日粮苜蓿草粉比例和蛋白水平及二者交互作用对豁眼鹅蛋黄铁锌含量的影响。结果表明,苜蓿草粉比例增加使蛋黄铁含量呈降低趋势,而日粮蛋白质水平对蛋黄铁含量无显著影响;日粮苜蓿草粉比例和蛋白质水平的交互作用对蛋黄铁含量无显著影响（P〉0.05）。苜蓿草粉比例增加使蛋黄锌含量呈增加趋势,而日粮蛋白质水平     

Iron Sources Effects on Growth,Physiological Parameters and Nutrition of Cacao

Productivity and sustainability of cacao (Theobroma cacao L.) in tropical soils are affected by levels of iron. Information is lacking on the cacao response to various sources of iron (Fe). A greenhouse experiment was conducted to evaluate the effects of five iron sources iron sulfate heptahydrate, ferric ethylenediamine-N,N’-bis(2-hydroxyphenylacetic acid), ferric diethylenetriaminepentaacetic acid, ferric ethylenediaminetetraacetic acid, fiesta herbicide (FeSO₄ · 7H₂O, FeEDDHA, FeDTPA, FeEDTA,) at 10 mg Fe kg^?1 soil on growth, photosynthesis, content of photosynthetic pigments and starch and macro- and micronutrient nutrition of cacao. The various iron sources had significant effects on shoot and root dry biomass accumulation, leaf chlorophyll a and b content, carotenoid levels, SPAD index and P_N. These parameters were significantly correlated with concentration, uptake, influx, and transport and use efficiency of Fe. In cacao net photosynthesis, stomatal conductance, internal carbon dioxide (CO₂)_, and transpiration in leaf level responded differently to the sources of Fe. Invariably, macro and micronutrient uptake, influx, transport, and use efficiency showed differential responses to sources of iron but significant effects were only observed for copper (Cu), Fe, manganese (Mn), and zinc (Zn). Overall, FeDTPA, FeEDTA and FeHEDTA could be the best sources of Fe in improving, growth, photosynthesis and macro and micro nutrition of cacao.     

与Fe(III) 共存的Fe(II) 分光光度法测定

Fe(Ⅱ)的含量及变化与土壤和沉积物的氧化还原性质关系密切。当与Fe(Ⅲ)共存时,Fe(Ⅱ)的测定往往受到干扰。本文研究了常用显色剂2,2’-联吡啶和菲洛嗪(Ferrozine)测定土壤Fe(Ⅱ)时存在的问题及解决办法。结果表明,Fe(Ⅲ)可与显色剂作用形成络合物,该络合物对Fe(Ⅱ)测定所用波段的光线具有吸收作用,从而使Fe(Ⅱ)浓度被过高估计。Fe(Ⅲ)对Fe(Ⅱ)测定的干扰程度与其浓度及所选显色剂有关。当以2,2’-联吡啶为显色剂时,单位浓度Fe(Ⅲ)(1.0 mg/L)将导致Fe(II)的测定值比实际值高0.012 mg/L;而当菲洛嗪为显色剂时,单位浓度Fe(Ⅲ)引起的Fe(Ⅱ)高估值在0.010～0.032 mg/L之间。F-能够抑制Fe(Ⅲ)-显色剂络合物的形成。当F-的加入量超过Fe(Ⅲ)的4倍时,F-能有效地消除Fe(Ⅲ)的干扰。实际样品的测定结果表明,改进的Fe(Ⅱ)分光光度法能够满足土壤及沉积物中Fe(II)的准确测定。     

农业生产中的铁锰平衡问题

本文根据对菠萝和水稻的研究,论述了土壤和植物体内铁与锰的关系,认为在植物体内铁与锰的比例应保持一个平衡的关系。如果锰多铁少、比例失调,作物的正常生长将受到危害。     

Effect of iron deficiency on the growth,development and grain yield of some selected upland rice genotypes in the rainforest

Abstract

Iron deficiency is a major production constraint of upland rice in the tropics despite is abundance in the soil. This investigation aimed to explicate the effect of iron deficiency on the growth, development, grain yield and its attributes of some selected upland rice in the rainforest. Field experiments were established at Africa Rice sub-Station, Ibadan, Nigeria. The treatments consisted of 35 upland rice genotypes and availability of iron in the soil (Fe-sufficient and Fe-deficient). The treatments were arranged in alpha lattice design with three replications. It was observed that upland rice sown in iron (Fe) deficient soils had significantly lower growth (plant height, number of tillers and seedling vigor), flowered later, with significantly lower yield attributes (1000 grain weight, filled grain) and grain yield than those sown in Fe-sufficient soils. Conversely, the number of unfilled grains were significantly higher in upland rice sown in Fe-deficient than those in sufficient soils. Percentage yield loss was in the range 98.00% to 22.95% for China best and Faro 65 respectively. Genotypes were identified to be tolerant (Faro 65, NERICA 3 and IRAT 109) and susceptible (Ofada 2, NERICA 5 and China Best) to Fe-deficiency based on their percentage grain yield loss. These evidences suggested that despite the increased phenology of upland rice sown in Fe-deficient soils their reproductive growth was suppressed through increased number of unfilled grains as witnessed in China Best and Faro 64.     

Studies on Nutrient Distribution in Some Zambian Soils with Special Reference to Sulphur Using GIS (Geographic Information Systems) I. Total Sulphur Distribution in Major Zambian Soils

Total sulphur content of some benchmark soils was evaluated by correlating with the contents of soil organic C and amorphous oxides (Al and Fe), and the particle size distribution. An equation model to calculate the content of total soil sulphur was first obtained by regression analysis. Introducing these chemical and physical data of all the map units except for the wetlands into the equation model, the sulphur level on a national scale was estimated for each soil mapping unit in the exploratory soil map of Zambia. Second, the total sulphur content was rated into 3 classes based on the frequency distribution of the total sulphur content in the benchmark soils. Finally, the rated total sulphur content was incorporated into the national soil map database of GIS to produce a map with the total sulphur content of Zambian soils. The extent of each class was calculated and the distribution of the areas was examined in relation to rainfall and soil formation.     

Redox potential of bulk soil and soil solution concentration of nitrate,manganese, iron,and sulfate in two Gleysols

While the reduction of nitrate‐N, Mn(III,IV), Fe(III), and sulfate‐S in soil has been studied intensively in the laboratory, field research has received only limited attention. This study investigated the relationship between redox potential (E_H) measured in bulk soil and concentrations of nitrate, Mn²⁺, Fe²⁺, and sulfate in the soil solution of two Gleysols differing in drainage status from the Marsh area of Schleswig‐Holstein, Northern Germany. The soils are silty‐sandy and developed from calcareous marine sediments. Redox potentials were monitored weekly with permanently installed Pt electrodes, and soil solution was obtained biweekly by ceramic suction cups from 10, 30, 60, and 150 cm depth over one year. Median E_H at 10, 30, 60, and 150 cm depths was 470, 410, 410, and 20 mV in the drained soil and 500, 480, 30, and –170 mV in the undrained soil, respectively. A decrease in E_H below critical values was accompanied in the soil solutions (pH 7.4 to 7.8) by disappearance of nitrate below 0 to 200 mV, appearance of Mn²⁺ below 350 mV, and Fe²⁺ below 0 to 50 mV. Both metals disappeared from soil solution after aeration. In the sulfide‐bearing environment of the 150 cm depth of the undrained soil, however, the sulfate concentrations were highest at such E_H values at which sulfate should be unstable. This discrepancy was reflected in the fact that at this depth bulk soil E_H was about 400 mV lower than soil solution E_H (250 mV). When investigating the dynamics of nitrate, Mn, and Fe in soils, bulk soil E_H provides semi‐quantitative information in terms of critical E_H ranges. However, in sulfidic soil environments the interpretation of E_H measured in bulk soil is uncertain.