光生物反应器中光衰减特征与螺旋藻生长动力学研究

分析了光照强度在光生物反应器中的分布特征，结果表明，当光波长及光传播的路径确定时，光生物反应器中光衰减特征主要受培养物生物量浓度的影响，由回归的模型对实验数据的拟合可分析光衰减特征与培养物生物量浓度的相关性，为光生物反应器中平均光照强度的确定奠定基础。在光生物反应器中，当营养底物和环境温度不是螺旋藻生长限制因子时，通过平均光照强度对螺旋藻比生长速率的影响分析，结果表明，在实验条件下，螺旋藻比生长速率与平均光照强度的动力学模型可用Aiba光生长抑制方程描述，光亲和系数Ks为238.29umol/(m^2.s)，光抑制系数Ki为0．00493s.m^2/umol，光生物反应器中螺旋藻生长的饱和光照强度出现在190－272umol/(m^2.s)的范围内。     

雪藻高密度连续培养中生物量和花生四烯酸的高产率

以 1 .4cm和 2 .8cm光径的平板光生物反应器 ,恒定高光强 [2 4 0 0 μE/(m2 ·s) ],通气、无菌高密度连续培养雪地绿藻 (简称雪藻 )。连续采收并补充等量新鲜培养液 ,当藻体生物量(以去灰分干重表示 ,AFDW)达恒态时 ,研究雪藻比生长速率 (SGR)、藻体的生物产量、总脂肪酸 (TFA)和花生四烯酸 (AA)产率。结果表明 ,尽管随着比生长速率增加 ,雪藻高密度连续培养体系的AA/TFA、TFA/AFDW和AA/AFDW三个指标有不同程度的降低 ,但生物产量、总脂肪酸及其花生四烯酸产出都相当高。 2 .8cm光径的平板光生物反应器中 ,雪藻SGR为0 .2d- 1 时 ,每平方米光照面积日获 35 .3gAFDW的高产量 ;SGR 0 .1 35d- 1 时 ,TFA产率最大 ,为7.0g/(m2 ·d) ,此时AA产率也最高 ,达 2 .6g/(m2 ·d)。尽管 1 .4cm光径的反应器的培养体积比前者下降了 5 0 % ,但细胞浓度明显提高 ,单位光照面积的AFDW和TFA最大日产率只下降了37.3%和 1 0 % ,分别为 2 2 .1和 6.3g/(m2 ·d) ,而AA的最大日产率也是 2 .6g/(m2 ·d)。结果还表明 ,氮或磷营养亏缺能明显提高雪藻AA含量的各项指标 ,同时高光强也有利于雪藻累积AA。     

纤细角毛藻的光生物反应器培养

采用正交实验的方法,在光生物反应器中对纤细角毛藻 Chaetoceros gracilis的生长进行了研究,结果表明:光照强度、通气率对藻体细胞的生长具有显著的影响,在通气培养条件下,当培养密度较高时,纤细角毛藻细胞不仅能耐受超高光照强度的照射,而且还可以获得很高的生长速度。本实验条件下, -1 7经过 5 d的培养,细胞的比生长速率﹑生物量产量和细胞密度分别达到了 0.74 d ﹑1.13 g/L和 8.1×10 /mL的较高水平。     

气升式藻类光生物反应器的应用研究

藻类是光合生物,在适当的光照条件下才能进行高效的光合作用和加快生长。同时,光合作用产生氧气,如造成溶解氧过饱和,又会降低光合产率。因此,在藻类光生物反应器的设计中,必需重视两个问题。其一是提高反应器的光照表面积与体积比,以提高光能利用效率;其二是气升式反应器要通过气流传动,提高藻类的光能利用效率和传质效率,同时防止培养液中溶解氧过饱和。近年来国内外研制的藻类光生物反应器多为管式［１,５］和板式反应器［４］。作者认为气升式反应器不仅占地面积小,而且有可能较好地兼顾上述藻类培养的基本要求。因此研制了１００Ｌ外照…     

环境因子对高盒形藻生长及其生化组成的影响

运用14C示踪法测定高盒形藻光合作用速率,并在实验室模拟条件下,研究光、营养盐和温度等环境因子对高盒形藻细胞生化组成的影响.结果表明,在常温和适宜的光照强度范围内,藻类光合作用速率随光强增加而增加,其光合产物碳水化合物和类脂物含量呈增加趋势,而蛋白质含量则降低.当介质氮磷比为16时,高盒形藻生长最佳,蛋白质合成的百分比最高.高盒形藻光合作用过程平均活化能14.32kJ/mol,在27℃左右有最高光合作用速率和最高的碳水化合物与蛋白质含量之比.     

红球藻藻株对光强适应及在工程培养中的应用

于2007～2008年在云南楚雄,利用叶绿素连续荧光分析等技术方法,对比研究了3株雨生红球藻藻株(Haematococcus pluvialis)(H_0、H_2、H_3)不同类型细胞对光强适应能力和光化学机制、生长速率和虾青素累积情况,对比研究了红球藻细胞转化过程的光化学特性与能量分配机制。结果表明,3株雨生红球藻游动细胞、绿色不动细胞和红色不动细胞光合作用对光强需求存在明显差异性,其中绿色游动细胞H_0、H_2和H_3光饱和点分别为750、1000、750 μmol/(m~2·s),绿色不动细胞H_0、H_2和H_3光饱和点分别为750、750、500 μmol/(m~2·s),而红色不动细胞H0、H_2和H_3的光饱和点分别为500、750、500 μmol/(m~2·s)。上述数据意味着红球藻光合作用对光强需求以游动阶段细胞最高,其次为绿色不动细胞,而红色不动细胞对光需求最弱;3株红球藻光合作用对光强需求的顺序为H_2H_0H_3。从实际培养效果来看,H_0藻株游动细胞在9月、11月到次年5月生长最好,其中4月、11月比生长速度为藻株H_3的2.19倍和2.17倍,而在6～8月和10月份中,藻株H_2生长比较迅速,但是藻株之间差异性相对较小。针对3株红球藻虾青素累积而言,1～2月、4月、6月、9月、11～12月藻株H0的虾青素含量最高,3月、5月更适宜H_3积累虾青素,其余7～8月和10月H_2藻株积累虾青素更多。综合雨生红球藻细胞生长和虾青素累积二个决定产量的主要因素,作者认为,在秋末、冬、春和夏初等温度和光照相对较低季节,选择藻株H_0规模化培养可获得更好的生产效果,而在光照较强、温度较高和多雨的夏季和秋初季节,应选择藻株H_2培养产量更高。     

坛紫菜叶状体营养细胞与生殖细胞叶绿素荧光特性比较

利用叶绿素荧光技术对坛紫菜(Porphyra haitanensis)叶状体营养细胞和生殖细胞的光能利用特性进行了比较。结果表明:坛紫菜叶状体营养细胞和雌性生殖细胞的实际量子效率(ΔF/Fm′)差异不明显,但显著高于雄性生殖细胞;快速光曲线测定表明雌、雄藻体营养细胞的最大相对电子传递速率(rETRmax)相近,但显著高于雄性生殖细胞;不同生殖细胞半饱和光强(Ik)无显著差异;在生长光强下,营养细胞和雌性生殖细胞rETR、光化学猝灭(qP)和非光化学猝灭(NPQ)差异不明显,而雄性生殖细胞rETR、qP等荧光参数均显著低于营养细胞和雌性生殖细胞。本文表明坛紫菜叶状体营养细胞和雌性生殖细胞具有较高的光能利用能力,能够将吸收的光能多数用于电子传递,而雄性生殖细胞对光能的利用能力较低。     

钝顶螺旋藻在LED光电板式光生物反应器中的培养研究

分析研究了ＬＥＤ集成光电板光辐射强度对螺旋藻生物量浓度、螺旋藻比生长速率、藻光合放氧量及藻光合色素等螺旋藻生长特性的影响，并分析了ＬＥＤ集成光电板辐射红光及红、蓝组合双波长光质与冷白荧光灯光质对藻类各有效组成部分的影响。结果表明，在光辐射强度尚未达到饱和光辐射强度之前，光辐射强度决定螺旋藻的比生长速度；超过饱和光辐射强度，光合作用产氧量趋向恒定，说明螺旋藻光合器官具有光合稳定性；与冷白荧光日光灯组相比，ＬＥＤ集成光电板射红光及红，蓝组合双波长光质非常适合螺旋藻的生长并促进细胞干重、叶绿素、藻胆蛋白的增加，在相同的光辐射强度[275.9μmol/(m^2.s)]下，采用ＬＥＤ集成光辐射板辐射单色红光与冷白荧光日光灯组相比，藻胆蛋白、藻细胞干重吸绿素a分别增加４３．３９％、９８．４０％，５１．５６３％。     

应用快速光曲线方法研究两株海洋超微型真核藻光合特性的差异

超微型浮游植物是海洋中重要的初级生产者,浮游植物吸收的光一部分用于光合作用,另一部分以荧光或热的形式耗散.本文利用调制叶绿素荧光仪（Pulse-Amplitude-Modulation,PAM）测定2株海洋超微型真核藻：细小微胞藻（Micromonas pusilla）和梨形脂金藻（Pinguiochrysis pyriformis）在不同光强下的叶绿素荧光和快速光曲线.结果表明细小微胞藻和梨形脂金藻在不同光强下的光系统II（PS II）的最大光量子产量（Fv/Fm）分别为0.572-0.634和0.624-0.426;最大相对电子传递速率（rETRmax）分别为61.58-163.56和76.69-143.17μmol/m2·s-1;半饱和光强（Ik）分别为212.37-946.00和307.44-671.28μmol·m-2·s-1;光能利用效率（α）分别为0.29-0.17和0.25-0.21.细小微胞藻和梨形脂金藻分别属于高光型和低光型的超微型浮游植物,光照条件会显著影响超微型浮游植物的光合特性,但不同类型的超微型浮游植物的光合特性对光的响应存在差异.     

温度和光径对微绿球藻生长及营养成分含量的影响

研究了温度和光生物反应器的光径对微绿球藻(Nannochloropsis oculata Hibberd)生长及细胞内几种营养成分含量的影响。结果表明,温度对微绿球藻的生长有显著影响(P0.05),对几种营养成分的含量有极显著影响(P0.01),在28℃的培养条件下,细胞生长速度最快,此时蛋白质含量最高,为5.66%,多糖含量最低,仅为1.47%,但最大生物产量却是在30℃的条件下获得,总脂与叶绿素a的含量随温度的升高而降低,类胡萝卜素含量随温度升高而增大。光生物反应器的光径对微绿球藻的生长和总脂、可溶性蛋白、色素的含量有极显著影响(P0.01),对多糖含量有显著影响(P0.05),比生长速率、最高细胞密度和单位体积产量均随光径的增大而减小,单位面积产量随光径的增大而增大;总脂、可溶性蛋白和多糖的含量随光径的增大而降低,叶绿素和类胡萝卜素含量随光径增大而增大,类胡萝卜素含量的增大趋势比叶绿素更明显。     

机载海洋激光雷达测量叶绿素a浓度、悬移质浓度和浅海深度的性能估计

以14:00时离水辐亮度作为背景光强度,模拟355nm激光雷达测量不同深度水层叶绿素a荧光的信噪比.分析体积衰减系数c、辐照度衰减系数k、散射系数b和透明度盘深度(SDD)的关系.最后模拟532nm激光雷达测量悬移质浓度的最大测量深度和误判率小于10%时的最大海底探测深度随SDD的变化.     

Simple estimation of penetration rate of light in intertidal sediments

A simple estimation of light penetration in tidal flat sediments was developed using various sediment size fractions and their attenuation rate of irradiance. The attenuation coefficients of the sediment size fractions of 63–125, 125–250, 250–500, 500–1000 μm and 1000–2000 μm were 8.10, 4.08, 2.92, 2.12 and 1.44 mm⁻¹, respectively. Using the average attenuation coefficient of the particle size fractions in the sediment, the calculated attenuation coefficient agreed well with the actual attenuation coefficient. The method presented gives a photo-parameter to predict productivity in intertidal sediments, given only the particle size fraction.     

海冰中侧向传播光衰减系数的解析验证

The attenuation of lateral propagating light(LPL) in sea ice was measured using an artificial light source in the Canadian Arctic during the 2007/2008 winter. The apparent attenuation coefficient μ(λ) for lateral propagating light was obtained from the measured logarithmic relative variation rate. In this study an analytical solution based on the strict optical theories is developed to validate the measured result. There is a good consistency between theoretical solution and measured data, by which a quite simple but very rigorous relationship among the light source, measurement geometry, and measured irradiance is established. The attenuation coefficients acquired by measurement and theory are the diffusion attenuation as an apparent optical property of ice, independent of the light source and shining condition. The attenuation ability of sea ice should be caused by the microstructure of sea ice, such as crystal size, ice density, brine volume, air inclusion, etc. It also includes the leak from both interfaces by directional scattering. It is verified that the measuring approach is operational and accurate to measure the attenuation of the LPL. The solution from this study did not tell the connection among the extinction and the inclusions of sea ice theoretically because of insufficient understanding.     

气升式光生物反应器培养裙带菜配子体的初步研究

在升气式光生物反应器中培养裙带菜配子体无性系。比生长速率最高为0.262d^－1，在快速生长期，日平均增重达到30％。通过在线测定DO和pH值变化实时了解配子体光合、呼吸作用的情况，通过测定碱度分析 子体对无机碳的利用情况，表明HCO3一直处于较高浓度，为配子体所利用的主要碳源。测定培养液的盐度、NO3^-和PO4^3-的浓度，其中NO3^-的利用量与配子体的生长相对应，而盐度变化可反映配子体对营养盐的作用。     

Variation of diffuse attenuation coefficient of downwelling irradiance in the Arctic Ocean

The diffuse attenuation coefficient(Kd) for downwelling irradiance is calculated from solar irradiance data measured in the Arctic Ocean during 3rd and 4th Chinese National Arctic Research Expedition(CHINARE), including 18 stations and nine stations selected for irradiance profiles in sea water respectively. In this study, the variation of attenuation coefficient in the Arctic Ocean was studied, and the following results were obtained. First, the relationship between attenuation coefficient and chlorophyll concentration in the Arctic Ocean has the form of a power function. The best fit is at 443 nm, and its determination coefficient is more than 0.7. With increasing wavelength, the determination coefficient decreases abruptly. At 550 nm, it even reaches a value lower than 0.2. However, the exponent fitted is only half of that adapted in low-latitude ocean because of the lower chlorophyll-specific absorption in the Arctic Ocean. The upshot was that, in the case of the same chlorophyll concentration, the attenuation caused by phytoplankton chlorophyll in the Arctic Ocean is lower than in low-latitude ocean. Second, the spectral model, which exhibits the relationship of attenuation coefficients between 490 nm and other wavelength, was built and provided a new method to estimate the attenuation coefficient at other wavelength, if the attenuation coefficient at 490 nm was known. Third, the impact factors on attenuation coefficient, including sea ice and sea water mass, were discussed. The influence of sea ice on attenuation coefficient is indirect and is determined through the control of entering solar radiation. The linear relationship between averaging sea ice concentration(ASIC, from 158 Julian day to observation day) and the depth of maximum chlorophyll is fitted by a simple linear equation. In addition, the sea water mass, such as the ACW(Alaskan Coastal Water), directly affects the amount of chlorophyll through taking more nutrient, and results in the higher attenuation coefficient in the layer of 30–60 m. Consequently, the spectral model of diffuse attenuation coefficient, the relationship between attenuation coefficient and chlorophyll and the linear relationship between the ASIC and the depth of maximum chlorophyll, together provide probability for simulating the process of diffuse attenuation coefficient during summer in the Arctic Ocean.     

利用光生物反应器培养雨生红球藻的研究初探

用光生物反应器与光照培养箱两种培养容器培养雨生红球藻(Haematococcus pluvialis),对雨生红球藻在两种容器培养过程中细胞生长、pH值、溶解氧(DO)及虾青素积累情况进行比较,同时比较不同接种密度对光生物反应器培养效果的影响。实验表明,光生物反应器中藻细胞的调整期较短,接种1 d后即进入指数生长阶段,在胁迫阶段则仅需4 d即达到虾青素含量的峰值;将pH值控制在偏碱性条件下(7.75±0.10)有利于藻细胞更好生长;营养培养阶段DO相对饱和度上升至80%,而在胁迫阶段则迅速降低,最低值小于6%;较高的接种密度(2.3×104个/mL)具有较短的营养培养周期(7 d),且因接种密度变化对胁迫周期长短无明显影响(均为4 d),选用较高的接种密度可望降低工业生产成本。     

Estimation of chlorophyll concentration from the specific fluorescence at 685nm in the upward irradiance just below the sea surface

An algorithm for estimating the chlorophyll concentration from the fluorescence intensity at 685nm in upward irradiance observed just below the sea surface is presented and discussed. The observed chlorophyll concentration is closely related to the ratio of the fluoresced quanta to the total incident quanta (downward plus upward quanta) in the spectral range between 350nm and 600nm. The correlation between them, however, is not good and the rate of increase of the ratio decreases as the chlorophyll concentration increases. This is due to the fact that the number of fluoresced quanta varies with attenuation of the incident light by various materials in the sea.A better correlation is obtained between the ratio of the fluoresced quanta to the upward quanta at wavelengths around 480nm. This is explained by the fact that dividing by the upward quanta at the appropriate wavelength compensates for apparent variation of fluorescence intensity with attenuation by the sea water. In this method, upward quanta at the four wavelengths of 480nm, 640nm, 685nm and 740nm are necessary for estimation of chlorophyll concentration. The quanta at 640nm and 740nm are used for interpolating the quanta at 685nm in the absence of fluorescence.It is also shown that the correlation of the observed chlorophyll concentration with the ratio of upward quanta at the wavelengths of 685nm and 480nm is also good. Use of this ratio is recommended for remote sensing of chlorophyll concentration since the number of spectral channels required by the remote multispectral imager can be minimized.     

大型海藻无性系微球体构建和反应器培养研究

利用大型海藻细胞的全能性获得了蜈蚣藻(Grateloupia filicina)、多管藻(Polysiphonia urceolata)和孔石莼(Ulva pertusa Kjellm)的无性系材料,在此基础上分别构建了绒球状微球体、网状微球体和簇生状微球体3种微球体形式,这种微球体形式适合于大型海藻的生物反应器高密度...     

Benthic photosynthesis in submerged Wadden Sea intertidal flats

In this study we compare benthic photosynthesis during inundation in coarse sand, fine sand, and mixed sediment (sand/mud) intertidal flats in the German Wadden Sea. In situ determinations of oxygen-, DIC- and nutrient fluxes in stirred benthic chamber incubations were combined with measurements of sedimentary chlorophyll, incident light intensity at the sediment surface and scalar irradiance within the sediment. During submergence, microphytobenthos was light limited at all study sites as indicated by rapid response of gross photosynthesis to increasing incident light at the sea floor. However, depth integrated scalar irradiance was 2 to 3 times higher in the sands than in the mud. Consequently, gross photosynthesis in the net autotrophic fine sand and coarse sand flats during inundation was on average 4 and 11 times higher than in the net heterotrophic mud flat, despite higher total chlorophyll concentration in mud. Benthic photosynthesis may be enhanced in intertidal sands during inundation due to: (1) higher light availability to the microphytobenthos in the sands compared to muds, (2) more efficient transport of photosynthesis-limiting solutes to the microalgae with pore water flows in the permeable sands, and (3) more active metabolic state and different life strategies of microphytobenthos inhabiting sands.     

Analysis of ocean color spectra (III)

The spectral measurements of the attenuation coefficient of sea water and the absorption coefficient of suspended particles and of yellow substance were made with a spectrophotometer for the sea waters sampled in Tokyo Bay. These parameters can be used to compute the expected spectral irradiance reflectance. Some relationships between the optical properties of sea water and the concentration of dissolved organic carbon, the dry weight of suspended matter and chlorophyll-a concentration are presented. On the basis of these results, the possibility of modelling the relationship between optical and material properties is discussed.