12 resultados para (-0.02)-0.08 phi

em Chinese Academy of Sciences Institutional Repositories Grid Portal


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采用XRD、FESEM-EDS、ICP及EIS等方法研究了Ti0.17Zr0.08V0.34Nb0.01Cr0.1Ni0.3氢化物电极合金微观结构和电化学性能。X射线衍射分析表明:该合金由体心立方结构(bcc)的V基固溶体主相和少量六方结构的C14型Laves相组成;FESEM及EDS分析表明:V基固溶体主相形成树枝晶,C14型Laves相呈网格状围绕着树枝晶的晶界,元素在两相中的分布呈现镜像关系。电化学性能测试结果表明:该合金的氢化物电极在303 ̄343K较宽的温度区间内,表现出较高的电化学容量,在303K和343K时,电化学容量分别为337.0mAh·g-1和327.9mAh·g-1。在303K循环100周后,容量为282.7mAh·g-1。ICP分析结果表明,氢化物电极在充放电循环过程中,V及Zr元素向KOH电解质中的溶出较为严重。EIS研究表明,金属氢化物电极表面电化学反应的电荷转移电阻(RT)随循环次数的增加而增加,相应的交换电流密度则随循环次数的增加而降低。氢化物电极循环过程中RT的增大以及V和Zr元素的溶解,可能是导致电极容量衰减的主要原因。

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Although studies on carbon burial in lake sediments have shown that lakes are disproportionately important carbon sinks, many studies on gaseous carbon exchange across the water-air interface have demonstrated that lakes are supersaturated with CO2 and CH4 causing a net release of CO2 and CH4 to the atmosphere. In order to more accurately estimate the net carbon source/sink function of lake ecosystems, a more comprehensive carbon budget is needed, especially for gaseous carbon exchange across the water-air interface. Using two methods, overall mass balance and gas exchange and carbon burial balance, we assessed the carbon source/sink function of Lake Donghu, a subtropical, eutrophic take, from April 2003 to March 2004. With the overall mass balance calculations, total carbon input was 14 905 t, total carbon output was 4950 1, and net carbon budget was +9955 t, suggesting that Lake Donghu was a great carbon sink. For the gas exchange and carbon burial balance, gaseous carbon (CO2 and CH4) emission across the water-air interface totaled 752 t while carbon burial in the lake sediment was 9477 t. The ratio of carbon emission into the atmosphere to carbon burial into the sediment was only 0.08. This low ratio indicates that Lake Donghu is a great carbon sink. Results showed good agreement between the two methods with both showing Lake Donghu to be a great carbon sink. This results from the high primary production of Lake Donghu, substantive allochthonous carbon inputs and intensive anthropogenic activity. Gaseous carbon emission accounted for about 15% of the total carbon output, indicating that the total output would be underestimated without including gaseous carbon exchange. (C) 2007 Elsevier Ltd. All rights reserved.

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Three large fish pens (0.36 km(2) of each) stocked with silver and bighead carp were set up in Meiliang Bay for controlling toxic Microcystis blooms. The responses of plankton communities and food consumption of silver and bighead carp were studied. Crustacean zooplankton were significantly suppressed in the fish pens. Total phytoplankton biomass, Microcystis biomass and microcystin concentration were lower in the fish pens than in the surrounding lake water, but the difference was not statistically significant. The present stocking density of silver plus bighead carp (about 40 g/m(3) in July) was likely too low to achieve an adequate control of Microcystis. Silver carp fed mainly on phytoplankton but bighead carp mainly on zooplankton: mean zooplankton contribution in the gut was 31.5% for silver carp and 64.7% for bighead carp. Compared with previous studies, both carp species preyed upon more zooplankton because of the abundant food resource. Daily rations of silver and bighead carp were estimated by Egger's model in the main growing season. Filtration rate was calculated from the daily ration and the density of plankton in the lake. During May-October, filtration rates of silver and bighead carp for phytoplankton were 0.22-1.53 L g(-1) h(-1) and 0.02-0.68 L g(-1) h(-1), respectively, and filtration rates for zooplankton were 0.24-0.44 L g(-1) h(-1) and 0.08-1.41 L g(-1) h(-1), respectively. Silver carp had a stronger ability of eliminating phytoplankton than bighead carp. To achieve a successful bioniampulation with a minimum effect of ichthyoeutrophication, the stocking proportion of bighead carp should be controlled in the future practice. (c) 2007 Elsevier B.V All rights reserved.

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This study investigated non-specific immune functions of the F-2 generation of "all-fish" growth hormone transgenic carp, Cyprinus carpio L. Lysozyme activity was 145.0 (+/- 30.7) U ml(-1) in the transgenic fish serum and 105.0 (+/- 38.7) U ml(-1) in age-matched non-transgenic control fish serum, a significant difference (P < 0.01). The serum bactericidal activity in the transgenics was significantly higher than that in the controls (P < 0.05), with the percentage serum killing of 59.5% (6.83%) and 50.8% (8.67%), respectively. Values for leukocrit and phagocytic percent of macrophages in head kidney were higher in transgenics than controls (P < 0.05). However, the phagocytic indices in the transgenics and the controls were not different. In addition, the mean body weight of the transgenics was 63.4 (6.65) g, much higher than that of the controls [39.2 (+/- 3.30) g, P < 0.01]. The absolute weight of spleen of the transgenics [0.13 (+/- 0.03) g] was higher than that of the controls [0.08 (+/- 0.02) g, P < 0.01]. However, there was no difference in the relative weight of spleen between the transgenics and the controls, with the spleen mass index being 0.21% (+/- 0.02%) and 0.20% (+/- 0.03%), respectively. This study suggests that the "all-fish" growth hormone transgene expression could stimulate not only the growth but also the non-specific immune functions of carp. (c) 2006 Published by Elsevier B.V.

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High quality YSi1.7 layers (chi(min) of Y is 3.5%) have been formed by 60 keV Y ion implantation in Si (111) substrates to a dose of 1.0 x 10(17)/cm(2) at 450 degrees C using channeled ion beam synthesis (CIBS). It shows that, compared to the conventional nonchanneled ion beam synthesis, CIBS is beneficial in forming YSi1.7 layers with better quality due to the lower defect density created in the implanted layer. Rutherford backscattering/channeling and x-ray diffraction have been used to study the structure and the strain of the YSi1.7 layers. The perpendicular and parallel elastic strains of the YSi1.7 epilayer are e(perpendicular to) = -0.67% +/- 0.02% and e(parallel to) = +1.04% +/- 0.08%. The phenomenon that a nearly zero mismatch of the YSi1.7/Si (111) system results in a nonpseudomorphic epilayer with a rather large parallel strain relative to the Si substrate (epsilon(parallel to) = +1.09%) is explained, and the model is further used to explain the elastic strain of epitaxial ErSi1.7 and GdSi1.7 rare-earth silicides. (C) 1998 American Vacuum Society.

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[I] 等离子体聚四氟乙烯的ESCA表征 本研究采用外部电容耦合式聚合装置,频率为13.56MHz,合成了等离子体聚四氟乙烯(PPTFE)。应用ESCA表征了辉光压和非辉光压产物的结构,同时应用CNDO进到了理论计算。结果表明,在辉光压上非辉光压中制得的PPTFE结构差别很大。非辉光内淀积物结构亦现差异。辉光压内的PPTFE是高度支化交联的,在本实验的典型反应条件下,PPTFE的F/C比为1.42,Gs区五个峰确定归属后,各主要对应基团的相对组成约为:CF_3-21%、CF_2-32%、CF-22%、-C from | to | of — 20%,其余为少量的CFH、CH_2(II)、CH_2(I)。在非辉光压内可得到近於线线型的PPTFE,其F/C为2.08,端基CF_3约占15%,CF_2占78%,代表支化交联的基团CF、-C from | to | of -皆为零,另外应用X射线衍射法证实,在非辉光压中形成的PPTFE具有类似于聚四氟乙烯的(PTFE)结晶,这一实验结果至今未见文献报导。深入分析这一结果,并运用ESR、MS、~(19)F-NMR等表征手段,进一步提出四氟乙烯等离子体聚合反应机理。这方面在[II]中论述。本工作提出五类十三种模型化合物,并运用Siegbahn的电荷电位模型同时结合使用CNDO/2电子计算机程序;还运用Pauling价键模型,分别应用这两种理论方法,计算了PPTFE中ClS结合能位移(ΔEi),所得结果相近,从而为ClS区五个峰的归属提供理论依据。五个峰归属为:(1) 284.7(ev) - CH_2(I),(2) 287.0(ev) - -C from | to | of -、CH_2(II),(3) 289.0(ev) -CF、CFH,(4) 291.5(ev) - CF_2,(5) 293.6(ev) - CF_3。通过对模型化合物中ClS的ΔEi计算结果,推导出F作为α、β、γ位碳上的取代基对α位碳上IS电子结合能位移影响所产生的效应值,并初步总结出表达这种效应的经验式:ΔEi = aα + bβ + cγ式中α、β、γ分别为2.23 ± 0.08(ev)、0.27 ± 0.02(ev)、0.20 ± 0.02(ev),a、b、c为取代基F的个数。实验结果还证明,淀积位置、功率、压力、等离子气体如Ar、He、N_2等反应条件对PPTFE膜结构有影响,并应用能量梯度解释这种影响;另外发现,同功率、同压力但不同淀积位置上以及同淀积位置但不同功率或不同压力时的PPTFE膜结构所受能量梯度的影响。本工作根据等离子体聚四氟工烯结构的表征结果,并结合ESR、MS等有关分析数据,提出了PPTFE的结构模型。[II] 等郭子体聚四氟乙烯的反应机理 鉴于等离子体聚合反应的复杂性,目前对等离子体聚合反应机理争论较大,其焦点是:反应的活性中心是离子还是自由基;反应地点是在气相还是在反应体系的固体表面。本工作通过对等离子体聚四氟乙烯气相产物的研究证实:等离子体聚合反就是通过自由基历程,引发和初级链增长主要在气相,脱F和支化交联反应在表面上进行。聚合反应装置同[I]中所述,聚合条件是功率60瓦,压力1 * 10~(-1)乇。通过液氟冷阱收集气相生成物,然后制备成有机溶液和本体溶液。气相生成物的ESR分析结果表明,PPTFE膜中存在自由基浓度约在10~(18)自旋数/克,峰形为一条反对称吸收线,宽为175G,g值是2.005。气相生成物的丙酮、苯、环已烷、已烷等有机溶液的ESR谱相同,皆为20条精细结构分裂谱线。另外,通过一系列实验,检测了桔黄色本体溶液的ESR谱,终于得到具有160条超精细结构的分裂谱线,自由基浓度高达10~(20)自旋数/克。初步认为是几种自由基的混合物,固谱图十分复杂,目前解谱尚有困难,需进一步研究。等高子体气相生成物中有大量自由基并且得到其精细和超精细分裂谱线,这一实验结果至今未见文献报导。这个结果进一步证实了聚合反应的活性中心主要是自由基。考察了PPTFE膜的自由基在90 ℃时随时间变化的ESR谱,发现一开始衰减很快;研究了PPTFE膜的自由基在不同气氛下常温衰减情况,结果指出:辉光压和非辉光压的PPTFE膜中自由基在空气中衰减快,辉光压的PPTFE膜中自由基在真空中及单体气氛中衰减缓慢。气相生成物的有机溶液在90 ℃时随时间变化的ESR谱表明,各峰衰减速率不同,证实并非一种自由基,溶液的自由基能与吡啶反应生成棕红色物质,可能是吡啶盐。本实验用GC-MS联用对气相冷凝物本体溶液进行了分析,比文献上只用MS与聚合反应体系联用分析气相混合物的方法,对分析反应机理提供更为有说服力的实验结果。结果表明,四氟乙烯等离子体聚合的气相生成物是直链的全氟烷烃(分子中碳原子数为C_3-C_8),还有含碳原子数为C_4、C_5、C_6、C_8全氟环烷烃,也可能是括分子链两端是自由基的直链全氟烷烃,还有二氟卡宾。从TFE等离子体聚合的气相中产生齐聚物及其结构特征,可以推断气相中发生了链引发反应和初级增长反应,引发反应的历程首先是TFE单体分子中π键断裂,其次是C~σ-C的σ键均裂,然后通过自由基的复合或诱导反应进行链的初级增长反应。还进行了气相生成物有机溶液的~(19)F-NMR分析,其结果初步看来与GC-MS的结果相一致。还探索了不同条件下在非辉光压内得到的PPTFE膜,进一步表明,在顺着气流方向的淀积位置上的膜结构是接近线型的。这个结果与用质谱、核磁的表征结果相符:从不用方面证实了上述反应历程。此外,通过对PPTFE及PTFE在Ar等离子体系中的刻蚀实验,表明了聚合膜上发生六量脱F反应。由这个结果并结合PPTFE膜及气相产物的结构表征,可以推测到PPTFE膜的支化,交联是通过表面反应进行的。综合四氟乙烯等离子体聚合反应机理的讨论,本论文建议了TFE的等离子体聚合反应历程模型。

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每种酸碱指示剂在其变色PH范围内都有一个明显的颜色变化,在其相应的PH-A曲线上总存在一段直线部分,通过选择一定PH变色范围和适当浓度的指示剂,就能使各指示剂PH-A曲线上的直线部分相互迭加成一条新的直线,从而加宽了混合指示剂的表现变色PH范围,依此原理,本论文以二种流动注射分析方法独立地完成了工艺流程中高浓定影液酸度的在线分析。并对这二种方法做了简单的对比。(一)工艺流程中高浓定影液酸度的在线分析方法研究(1)我们选择了内含0.08%溴甲酚紫,0.04%溴百里酚兰,0.02%甲酚红组成的混合指示剂的6%稀释液作为试剂,以C-41CX定影浓缩液作载流,用F2A-分光光度法完成了高浓度定影液酸度的在线测定,相对标准偏差在50.2%以内,采样频率为100次/h,分析周期很短(25秒),在5.5~8.0PH范围内,PH-A工作曲线具有很好的线性关系,相关系数0.9996,斜率即灵敏度达到:0.198A/PH。(二)工艺流程中高浓定影液酸遮掩在线分析方法研究(2)我们造反了0.005%的溴甲酚紫,0.009%的溴百里酚兰和0.025%的甲酚红作为混合酸碱指示剂,以蒸馏水作载流,通过选择最佳测定条件用流动注射-分光光度法(F2A-Spectrophotometry)在线测定了不宜用其它分析法测定的高浓溶液的酸度。该分析方法还可以推广到其它高浓溶液的酸度的在线测定。相对误差在±0.2%以内;分析周期为30秒;采样体积为60μL。在5.2~8.5PH范围内,混合指示剂的PH-A工作曲线具有良好的线性关系,相关系数达到0.9991,工作曲线斜率即是灵敏度达到0.376A/PH。

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ErSi1.7 layers with high crystalline quality (chi(min) of Er is 1.5%) have been formed by 90 keV Er ion implantation to a dose of 1.6X10(17)/cm(2) at 450 degrees C using channeled implantation. The perpendicular and parallel elastic strain e(perpendicular to)=-0.94%+/-0.02% and e(parallel to)=1.24%+/-0.08% of the heteroepitaxial erbium silicide layers have been measured with symmetric and asymmetric x-ray reflections using a double-crystal x-ray diffractometer. The deduced tetragonal distortion e(T(XRD))=e(parallel to)-e(perpendicular to)=2.18%+/-0.10%, which is consistent with the value e(T(RBS))2.14+/-0.17% deduced from the Rutherford backscattering and channeling measurements. The quasipseudomorphic growth of the epilayer and the stiffness along a and c axes of the epilayer deduced from the x-ray diffraction are discussed.

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The structural properties of Semi-insulating gallium arsenide (SI-GaAs) crystal grown with power-travelling technique in space have been studied by double-crystal x-ray diffractometry and chemical etching. The quality of the crystal was first evaluated by x-ray rocking-curve method. The full width at half maximum of x-ray rocking curve in space-grown SI-GaAs is 9.4+/-0.08 are seconds. The average density of dislocations revealed by molten KOH is 2.0 X 10(4) cm(-2), and the highest density is 3.1 X 10(4) cm(-2). The stoichiometry in the single crystal grown in space is improved as well. Unfortunately, the rear of the ingot grown in space is polycrystalline owing to being out of control of power. (C) 1999 COSPAR. Published by Elsevier Science Ltd.

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采用两步加热高温固相法合成了掺杂Nd3+的LiFe1-xNdxPO4/C复合材料(x=0,0.01,0.02,0.04,0.06,0.08)。用TG-DSC对前驱体进行分析和SQUID(超导量子干涉仪)对样品中Fe3+的磁性测定,优化了合成工艺条件;采用XRD、FE-SEM、EDS等方法分析了样品的结构并对其电化学性能进行了测试。结果表明:LiFe1-xNdxPO4/C复合材料具有橄榄石型结构;当Nd3+的掺杂量6%(物质的量分数)、煅烧温度700℃、煅烧时间16 h时,样品在0.2C(1C=170.0 mA.g-1)电流密度下的最大放电比容量可达165.2 mAh.g-1,循环100次后的容量保持率仍为92.8%,在1C、2C、5C下的最大放电比容量分别为146.8、125.7和114.8 mAh.g-1。通过测定样品在不同较低倍率下的放电比容量,采用外推法得出制备样品的实测理论比容量为168.7 mAh.g-1。

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在基础饲料中分别添加0.04%低聚木糖、0.13%酵母细胞壁、0.08%胆汁酸和同量组合添加,形成5个处理组。采用随机区组试验设计,将体重151.3±15.2 g 的健康大菱鲆鱼165尾平均分配到5个处理组(A~E)中(每组3重复),经72天试验,进行了生长、水质、消化、免疫等试验和测定,结果如下: 组合组的生长效果和饲料利用率最好,酵母细胞壁或低聚木糖单独添加,表现出优良的促生长和饲料利用率;单独添加胆汁酸也有良好效果。4试验组(组合组、酵母细胞壁组、低聚木糖组、胆汁酸组)与对照组比较,增重率分别提高15.4%、13.9%、12.4%(p<0.05)和7.4%(P>0.05),饲料系数分别降低6.9%、6.2%、5.4%(p<0.05)和3.8%(P>0.05)。 不同添加剂及组合对试验鱼所处水环境因子变化仅有小幅影响,统计差异不显著(p>0.05)。4试验组比对照组的水体氨氮含量分别提高4.0%、3.2%、3.0%和0.8%(P>0.05),COD含量分别提高2.8%、-2.2%、-3.4%和0.8%(P>0.05)。根据试验结果,建议水环境因子(氨氮、磷酸盐、COD等)作为水产动物营养与饲料研究的主要衡量指标之一。 3种添加剂组合后达到提高生长大菱鲆非特异性免疫功能的最优效果,对补体C3和C4、细胞吞噬活力和SOD的提高作用尤为显著;酵母细胞壁单独添加对补体C3和细胞吞噬活力的作用更加显著;低聚木糖单独添加对补体C4和细胞吞噬活力的作用显著;单独添加胆汁酸提高免疫力的作用相对较弱。 4试验组比对照组的蛋白质消化酶活力在胃和前肠,分别提高20%和24%、17%和19%、16%和15%(p<0.05)、11%和3%(P>0.05);脂肪消化酶活力在前肠和中肠,分别提高22%和19%、19%和17%(p<0.05)、7%和12%(p>0.05)、19%和18%(p<0.05)。 4试验组比对照组的蛋白质消化率分别提高了3.6%、2.9%、3.7%(p<0.05)和1.5%(p>0.05);粪蛋白质排出量减少12.7%、7.1%、13.4%和2.4%(p>0.05)。说明,3种添加剂显著提高了生长大菱鲆蛋白质消化率,使粪蛋白质排出量不同程度降低,显示了试验使用添加剂的无公害效应。 权衡不同添加剂及其组合对大菱鲆生长期生长性能、饲料利用率、水生态因子、消化酶活力、非特异性免疫、蛋白质消化与粪蛋白质排出的综合影响,本研究从生态与环保角度得出:3种添加剂组合的效果最好,酵母细胞壁或低聚木糖单独添加表现出优良效果;单独添加胆汁酸也有良好作用。

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湖泊生态系统是陆地水体生态系统的重要组成部分。随着社会经济的不断发展,各种人为因素对湖泊生态系统的影响日益突出,打破了其自然演变规律,诸如 “二次污染”、水体富营养化、重金属污染等环境问题接踵而来。而铁是水生生态系统初级生产力所必需的重要微量营养元素之一,在一定的条件下可以控制和影响浮游藻类的生长速度和种类;而且,铁的氧化还原敏感性很强,其价态的改变往往会影响其它相关重金属的迁移和转化。因此,湖泊生态系统中铁的生物地球化学循环研究具有非常重要的意义。近年来的研究显示,铁同位素分析技术可以用于各种生物作用和非生物作用过程的研究,在海洋和河流生态系统中已有广泛的应用,而对湖泊生态系统的研究则鲜见报导。乌江流域中等富营养化的湖泊――红枫湖和贵阳西南郊矿化程度较高的湖泊――阿哈湖是研究湖泊生态系统中铁生物地球化学循环的理想场所。本文选取这两个性质不同的湖泊为研究对象,运用硫同位素、铁同位素及重金属和营养盐等地球化学方法手段,对两湖流域内硫酸盐的来源、硫同位素的季节和剖面变化特征、铁的来源及铁同位素组成的季节和剖面变化特征及其控制和影响因素等进行了研究和探讨,进一步完善了铁同位素分馏机理,为深化理解和研究湖泊生态系统中铁和硫的生物地球化学循环提供一定的科学依据。论文所获的主要认识总结如下: 两湖流域内湖水与河水的硫酸盐硫同位素地球化学 (1)阿哈湖流域和红枫湖流域水体的硫酸盐浓度和δ34S值均有较宽的分布范围。各入湖支流中,受煤矿废水或煤矸石淋溶液污染的河水的δ34S值相对较低(-8.10‰~-14.92‰),而受生活污水影响严重的河水则具有相对较高的δ34S值(-5.68‰~+0.88‰)。相比而言,阿哈湖流域水体纳入了大量的煤矿废水和煤矸石淋溶液,硫污染程度较红枫湖流域更为严重。因此,阿哈湖湖水具有相对较高的硫酸根浓度(平均为2.30 mmol.L-1)和相对较低的δ34S值(平均为-8.10‰),而红枫湖则具有相对较低的硫酸根浓度(平均为0.96 mmol.L-1)和相对较高的δ34S值(平均为-6.80‰)。 (2)阿哈湖湖水中的硫酸盐主要受煤矿废水、煤矸石淋溶液以及雨水等的控制;红枫湖湖水的硫酸盐主要来源于煤中黄铁矿的氧化和雨水输入,土壤硫化物的氧化和蒸发岩的溶解对湖水硫酸盐硫同位素组成的贡献较小。相比之下,雨水对红枫湖湖水硫同位素的影响更为明显。 (3)红枫湖和阿哈湖湖水的硫酸盐的δ34S值均具有明显的剖面变化特征,而且两湖的变化趋势相似,总体表现为,夏秋季节表层湖水和底层湖水的δ34S值相对较高,而冬春季节湖水剖面上下几乎没有变化。湖水硫酸盐浓度也呈现类似的变化特征,这主要与季节性厌氧湖泊夏季分层冬季混和的典型特点有关。夏季湖水分层期间,大量降雨在湖泊表层的滞留使得δ34S值升高而硫酸盐浓度降低,湖泊底部水层中硫酸盐细菌的还原作用使得底层湖水的硫酸盐浓度降低,而δ34S值升高。 两湖流域内铁同位素地球化学 (1)阿哈湖流域各类样品的δ56Fe值分布在-2.03‰~+0.12‰之间,分布范围较宽。其中湖水悬浮颗粒物的δ56Fe值在-1.36‰~-0.03‰之间,整体相对偏负。湖周各支流河水悬浮颗粒物的δ56Fe值在-0.88‰~+0.07‰之间,也相对富集轻的铁同位素;湖底沉积物和孔隙水的δ56Fe值的分布范围分别为-1.75‰~-0.59‰和-2.03‰~+0.12‰;大气颗粒物和浮游藻类的δ56Fe值分别为+0.06±0.02‰和+0.08‰。与阿哈湖相比,红枫湖流域各类样品的δ56Fe值的分布范围相对较窄,在-0.92‰~+0.36‰之间。湖水悬浮颗粒物的δ56Fe值在-0.85‰~+0.14‰之间,河水悬浮颗粒物的铁同位素组成变化范围为-0.89‰~+0.10‰,二者的变化范围相似。红枫湖沉积物的δ56Fe值在-0.18‰~+0.08‰之间,明显比阿哈湖沉积物的铁同位素组成偏正;而对应孔隙水的铁同位素组成的变化范围为-0.59‰~-0.24‰,均要比对应沉积物的铁同位素值要低。藻类和鲫鱼鱼肉的δ56Fe值分别为+0.36‰和-0.92‰。 (2)通过对两湖研究区湖水悬浮颗粒物与各输入端员环境样品的铁同位素值的研究表明,湖水悬浮颗粒物的δ56Fe值不仅受各输入端员的控制和影响,湖泊内部相关的生物地球化学过程也对湖水悬浮颗粒物的铁同位素组成变化产生了重要影响。两湖研究区内湖水悬浮颗粒物的铁同位素组成均存在季节变化特征,但受湖泊自身特点的影响,主要控制因素方面存在一定差异。夏季阿哈湖湖水悬浮颗粒物的铁同位素值变幅较大,其变化主要表现在表层和底层。表层因受陆源输入的有机结合态铁的影响而具有较负的δ56Fe值,而大气沉降颗粒物和湖泊表层的浮游藻类的影响并不显著。夏季湖水分层期间,“Ferrous Wheel”铁循环对于界面附近铁同位素的重分配起到了主要的控制和影响作用,湖水悬浮颗粒物的铁同位素值在氧化-还原界面附近达到了极负值。水-沉积物界面附近滞水层中亚铁类硫化物的生成可能也是水-沉积物界面附近水层内颗粒物的δ56Fe值偏负的原因之一。而冬季湖水混和时期,阿哈湖湖水剖面悬浮颗粒物的δ56Fe值的变幅明显减小。与阿哈湖不同,藻类的吸附作用可能在夏季红枫湖上层水体中占有主导地位,其湖水悬浮颗粒物的铁同位素组成随叶绿素水平的降低而逐渐降低。下层湖水悬浮颗粒物的铁同位素组成变化也受“Ferrous Wheel”铁循环的影响,在红枫湖后五剖面 20m 处达到-0.18‰,大坝剖面底层约为-0.46‰,其变幅没有阿哈湖悬浮颗粒物的δ56Fe值大,可能是受到了湖水中大量有机物质的影响。冬季红枫湖后五剖面的变化趋势与夏季相似,上层和下层水体悬浮颗粒物分别受不同影响因素的控制。上层水体悬浮颗粒物的铁同位素变化不明显,与Fe、Al、Mn、Zn、Co等元素的含量呈现良好的正相关关系;而底层水体悬浮颗粒物的δ56Fe值变幅比夏季要大,HW采样点20m处可达-0.85‰,与Fe、Al、Zn、Co等呈现良好的负相关关系,具体影响因素还有待于进一步研究。