Regulation of photosynthetic electron transport and photophosphorylation in intact chloroplasts and leaves of Spinacia oleracea L.

Oxygen ist reduced by the electron transport chain of chloroplasts during CO₂ reduction. The rate of electron flow to oxygen is low. Since antimycin A inhibited CO₂-dependent oxygen evolution, it is concluded that cyclic photophosphorylation contributes ATP to photosynthesis in chloroplasts which cannot satisfy the ATP requirement of CO₂ reduction by electron flow to NADP and to oxygen. Inhibition of photosynthesis by antimycin A was more significant at high than at low light intensities suggesting that cyclic photophosphorylation contributes to photosynthesis particularly at high intensities. Cyclic electron flow in intact chloroplasts is under the control of electron acceptors. At low light intensities or under far-red illumination it is decreased by substrates which accept electrons from photosystem I such as oxaloacetate, nitrite or oxygen. Obviously, the cyclic electron transport pathway is sensitive to electron drainage. In the absence of electron acceptors, cyclic electron flow is supported by far-red illumination and inhibited by red light. The inhibition by light exciting photosystem II demonstrated that the cyclic electron transport pathway is accessible to electrons from photosystem II. Inhibition can be relieved by oxygen which appears to prevent over-reduction of electron carriers of the cyclic pathway and thus has an important regulatory function. The data show that cyclic electron transport is under delicate redox control. Inhibition is caused both by excessive oxidation and by over-reduction of electron carriers of the pathway.     

Temporal variations in metal enrichment in suspended particulate matter during rainfall events in a rural stream

We studied enrichment of heavy metals (V, Zn, Cr, Ni, Cu, Pb, As, Sb, and Cd) in a rural stream of the Kuji River basin in central Japan in suspended particulate matter, and associated transport flux during two rainfall events (in November 2003 and in April 2008). The concentration of heavy metals in suspended particulate matter (SPM) exhibited a distinctive temporal variation, wherein the concentrations decreased with increasing water discharge and then increased as the discharge decreased. Concentration of dissolved metal forms showed a slight increase with scatters around the flow rate peak. Enrichment factors for those metals in the SPM decreased sharply as the flow rate increased, making an obvious concave shaped curve (the November 2003 rainfall event). The metal enrichment factors under low flow conditions had a similarity to those found in atmospheric deposits at a foot of the Kuji River basin, suggesting atmospheric source would contribute to enriching the SPM with those metals in part. Mineralogical analyses and carbon content analysis (the April 2008 rainfall event) of the SPM suggests the SPM matrix became more lithological as the flow rate increased. The changes observed in the matrix are thought to be directly related to progressive changes in metal enrichment within the SPM. Concerning the transport phase of several heavy metals, a dynamic change in transport phase partitioning within a rainfall event was suggested. The present enrichment factor study and the SPM matrix characterization implied the partitioning change is due to an increase in lithologic solids during high flow conditions.     

The reduction of artificial electron acceptors at sub-zero temperatures by chloroplasts suspended in fluid media.

1. Chloroplasts can be suspended in aqueous/organic mixtures which are liquid at sub-zero temperatures with a good retention of the ability to reduce artificial electron acceptors. The reduction of ferricyanide and 2,6-dichlorophenolindophenol at temperatures above 0 degrees C is about 50% inhibited by 50% (v/v) ethylene glycol. Higher concentrations cause more extensive inhibition. 2. Different solvents were compared on the basis of their ability to cause a given depression of the freezing point of an aqueous solution. Ethylene glycol caused less inhibition of electron transport than glycerol, which in turn was found to be superior to methanol. 3. The reduction of oxidised 2,3,5,6-tetramethyl-p-phenylenediamine could be measured at -25 degrees C in 40% (v/v) ethylene glycol. Using an acceptor with a high extinction coefficient, methyl purple (a derivative of 2,6-dichlorophenolindophenol) it was possible to observe electron flow at temperatures as low as -40 degrees C in 50% (v/v) ethylene glycol. 4. From studies of the effects of the inhibitors 3(3,4-dichlorophenyl)-1,1-dimethylurea and 2,5-dibromo-3-methyl-6-isopropyl-p-benzoquinone it is suggested that electron flow from the donor side of Photosystem II to the acceptor side of Photosystem I can occur at temperatures at least as low as -25 degrees C. The ultimate electron donor is presumably water but it was not possible to demonstrate this directly.     

青藏高原沙柳河流域自然径流驱动的流域生物信息流量化特征——以环境微生物为指标

物质流、能量流、信息流是生态系统过程研究中的三大主题。然而，在流域生态学研究中，有关信息流的研究一直缺位。为了推动流域信息流研究，从生物信息流切入，提出"流域生物信息流"概念，将其定义为"生物信息依托于流域生态系统过程在不同空间和系统之间进行传递、交流、作用、反馈的路径、过程与控制"，并将其研究内容拟定为主要关注于水陆间、干支流间、上下游间、不同生态斑块间的流域生物信息流及其周期性节律和趋势性变迁，以及地貌、水文、人类活动等对这些生物信息流的影响等。然后，以青藏高原上青海湖重要入湖河流--沙柳河的河流水体微生物和岸带土壤微生物为研究对象，利用环境DNA技术，对沙柳河流域的自然径流驱动的流域生物信息流进行量化研究。结果表明（1）岸带土壤到水体的流域生物信息流主要由地表表面流、地下潜流等驱动，并受环境过滤效应影响，其输移效率降雨天约为62.76%、晴天约为44.16%，其中输移能力降雨天约为68.49%、晴天约为56.82%，环境过滤效应降雨天约为8.38%、晴天约为22.28%；（2）水体上游到下游的流域生物信息流主要由河川径流驱动，并受衰减效应影响，其基础综合输移效率约为97.41%/km，其中径流输移能力约为99.42%/km，无效流域生物信息流占比约为43.46%，无效流域生物信息流的半衰距离约为14.52 km；（3）降雨通过增加地表表面流等的冲蚀搬运能力并削弱环境过滤效应，促使岸带土壤到水体的流域生物信息流输移能力和输移效率增大；（4）流域生物信息流的输入在一定程度上增加了输入地的可检出生物多样性，但这种增加对于流水生态系统来讲是非累积的。     

Hydrological Response to Climate Change for Gilgel Abay River,in the Lake Tana Basin - Upper Blue Nile Basin of Ethiopia

Climate change is likely to have severe effects on water availability in Ethiopia. The aim of the present study was to assess the impact of climate change on the Gilgel Abay River, Upper Blue Nile Basin. The Statistical Downscaling Tool (SDSM) was used to downscale the HadCM3 (Hadley centre Climate Model 3) Global Circulation Model (GCM) scenario data into finer scale resolution. The Soil and Water Assessment Tool (SWAT) was set up, calibrated, and validated. SDSM downscaled climate outputs were used as an input to the SWAT model. The climate projection analysis was done by dividing the period 2010-2100 into three time windows with each 30 years of data. The period 1990-2001 was taken as the baseline period against which comparison was made. Results showed that annual mean precipitation may decrease in the first 30-year period but increase in the following two 30-year periods. The decrease in mean monthly precipitation may be as much as about -30% during 2010-2040 but the increase may be more than +30% in 2070-2100. The impact of climate change may cause a decrease in mean monthly flow volume between -40% to -50% during 2010-2040 but may increase by more than the double during 2070-2100. Climate change appears to have negligible effect on low flow conditions of the river. Seasonal mean flow volume, however, may increase by more than the double and +30% to +40% for the Belg (small rainy season) and Kiremit (main rainy season) periods, respectively. Overall, it appears that climate change will result in an annual increase in flow volume for the Gilgel Abay River. The increase in flow is likely to have considerable importance for local small scale irrigation activities. Moreover, it will help harnessing a significant amount of water for ongoing dam projects in the Gilgel Abay River Basin.     

Cyanide-insensitive oxidation of ascorbate + NNN''N''-tetramethyl-p-phenylenediamine mixture by mung-bean (Phaseolus aureus) mitochondria. An energy-linked function.

Freshly prepared washed or purified mung-bean (Phaseolus aureus) mitochondria utilize oxygen with ascorbate/tetramethyl-p-phenylenediamine mixture as electron donor in the presence of KCN. ATP control of the oxygen uptake can be observed with very fresh mitochondria. The electron flow, which is inhibited by antimycin A, salicylhydroxamic acid or octylguanidine, takes place by reversed electron transport through phosphorylation site II and thence to oxygen through the cyanide-insensitive pathway. Oligomycin and low concentrations of uncoupler partially inhibit the oxygen uptake in a manner similar to that observed for other energy-linked functions of plant mitochondria. An antimycin A-insensitive oxygen uptake occurs if high concentrations of uncoupler are used, indicating that the pathway of electron flow has been altered. The process of cyanide-insensitive ascorbate oxidation is self-starting, and, since it occurs in the presence of oligomycin, it is concluded that the reaction can be energized by a single energy-conservation site associated with the cyanide-insensitive oxidase pathway.     

Extreme hydrologic banding in a large-river Floodplain, California, U.S.A.

Where tributaries meet, certain conditions of flow and topography often result in incomplete mixing and the formation of spatially and temporally persistent plumes or bands. Yolo Bypass, the primary floodplain of the lower Sacramento River (California, USA), provides an extreme example of this effect. Inspection of recent and historical aerial photographs revealed that the four major tributaries of Yolo Bypass typically do not substantially mix laterally within the floodplain. The phenomenon is notable in the number of tributaries involved (4), the distance over which the bands remain distinct (>61 km), and the persistence of the bands despite channel constrictions and long cross-wind fetch. This effect demonstrates the importance of lateral variability during floodplain flow events, including transport and distribution of chemical constituents, and habitat for fish and other organisms that use floodplains as migration corridors and rearing areas. Handling editor: S. M. Thomaz     

Interim Response of Dissolved Oxygen to Reestablished Flow in the Kissimmee River,Florida, U.S.A.

Restoration of the Kissimmee River should have multiple ecological benefits including improved dissolved oxygen (DO) within the river channel. Channelization of the Kissimmee River virtually eliminated flow through the natural river channel. After channelization, chronically low DO concentrations were observed in the stagnant remnant channel. Although no DO data from before channelization exist, reference estimates of pre‐channelization conditions were derived from seven relatively unimpacted streams. Stations along the Kissimmee River were sampled for 3 years before construction of the first phase of the restoration project began and for up to 8 years after the completion of construction. After Phase I construction, DO concentrations in the area of the river channel to which flow had been restored increased significantly from 2.2 to 4.9 mg/L, which is similar to DO concentrations observed in the reference streams. Mean DO concentrations for the reference streams ranged from 4.6 to 6.7 mg/L. Comparison of reference data to data from the pre‐Phase I and post‐Phase I system suggests that channelization had a negative impact on DO and that DO concentrations in the post‐Phase I Kissimmee River channel have made a significant recovery. Long‐term data trends demonstrate that DO concentrations can be negatively impacted by high flow events and that recovery from these events is generally quick, suggesting some degree of resilience in the system.     

Intracellular transport in axonal microtubular domains II. Velocity profile and energetics of circumtubular flow

Summary The microtubule is a highly efficient vectorial structure that could orient a transport force generating mechanism and also absorb the recoil produced by vectorial force generation. We have assumed that a nonspecific shear force is generated in a narrow annulus around the microtubule and have calculated the velocity profiles in the shear flow and drag flow regions that result from such a mechanism. This circumtubular flow of low visocosity cytoplasm is thought to be the basic carrier stream that produces the observed axoplasmic transport phenomena. These carrier streams are devoid of neurofilaments and form the halos or exclusion zones seen around microtubules in electron micrographs. Individual carrier streams may merge hydrodynamically to produce transport domains that are capable of moving large organelles in a saltatory manner. Exchange of material between the low viscosity transport domains and the high macroviscosity neurofilament regions produces mass fluxes akin to those found in chromatographic columns. Calculations of energy required to maintain streaming and of the energy available to the transport system show a close correspondence and demonstrate that a continuous carrier stream activity is energetically feasible.     

Population genetic structure of Vitex negundo (Verbenaceae) in Three-Gorge Area of the Yangtze River: The riverine barrier to seed dispersal in plants

Previous studies have demonstrated that large rivers can influence inter- and intra-specific gene flow for many animals. The effects of large rivers on the genetics of plant populations have focused on either hydrochoric impacts of water current on gene flow or genetic differentiation among populations from different watersheds. Few studies have explicitly tested the barrier effects on plant gene flow across banks of large rivers, especially their relative effects on pollen and seed dispersals. The Yangtze River (Changjiang River), one of the major rivers of the world, provides an excellent model to evaluate the impacts of rivers on gene flow in plants. Using RAPD (random amplified polymorphic DNA) and cpDNA (chloroplast DNA) markers, we investigated the genetic structure of 10 populations of Vitex negundo in two regions of Three-Gorge Area along the Yangtze River. Each region contained two populations on the north bank, two on the south bank and one island population along the river. The analyses indicated low RAPD between banks, and similar or a little higher differentiation between populations within the same bank. In contrast, a large proportion of chloroplast polymorphism was ascribed to among-bank variation but much lower cpDNA differentiation was among populations within the same bank. These results indicate that the Yangtze River represents a general barrier to the dispersal of seeds but not to the movement of pollen in V. negundo. The cpDNA genetic distances or differentiations between the island populations and those on either bank of the river are intermediate to those between the banks across the river, implying that the islands in the Yangtze River may serve as a stepping-stone for seed dispersal. Our results suggest that large rivers may serve as a general barrier, not only for the movement of animals, but also for the dispersal of plants, which should be of great significance for the conservation of biodiversity around the rivers.     

Potential environmental impacts associated with the proposed abstraction of water from the Okavango River in Namibia

The Namibian Department of Water Affairs has in the past faced considerable pressure to relieve the water shortages caused by recent droughts. One of the options considered in 1996, following poor runoff during the 1994/95 and 1995/96 seasons, was a proposal to abstract some 17Mm³ of water per year from the Okavango River at Rundu, and transfer this via a 260km long pipeline to the head of the Eastern National Water Carrier at the town of Grootfontein. Part of the overall evaluation of this scheme included an assessment of the potential environmental impacts that could arise. An initial environmental evaluation was conducted from a point approximately 40 kilometres upstream of Rundu in Namibia, to the distal end of the Okavango Delta at Maun in Botswana.

Hydrological studies showed that the proposed abstraction represented a reduction of approximately 0.32% in the mean annual flow of the Okavango River at Rundu. The abstraction represents 0.17% of the mean annual flow at Mukwe, downstream of the Cuito River confluence. The adverse effects of the proposed water abstraction scheme would be extremely small along the Okavango River in Namibia, whilst outflows from the lower end of the Okavango Delta to the Thamalakane River would be reduced by some 1.44Mm³/year (11%). Additional studies showed that these effects could be reduced by some 10–13% if abstraction was confined to the falling limb of the hydrograph.

Hydrological simulations have shown that the maximum likely loss of inundated area in the Okavango Delta would total approximately 7km² out of some 8 000km². This potential loss in inundated area would be concentrated in the lower reaches of the seasonal swamps and seasonally inundated grasslands, specifically in the lower reaches of the Boro, Gomoti, Santantadibe and Thaoge channels. However, these effects would most likely be expressed as a shoreline effect, with the loss in area spread out over the shoreline and periphery of islands and would not be restricted to a single specific area. This anticipated loss in inundated area is unlikely to have measurable impacts on environmental components.

Overall, the study found no 'fatal flaws' which would prevent the water abstraction scheme from proceeding and the anticipated effects on the Okavango system are more likely to be seen in the Okavango Delta, rather than along the Okavango River. The anticipated ecological implications of the scheme were small in spatial extent and are unlikely to be perceptible against the natural year-to-year variability in inundation of the Okavango Delta or outflows to the Thamalakane River. However, the public perceptions of the proposed water transfer project were strongly negative and appeared to be at least in part due to the very low water levels in the Okavango River and Okavango Delta during the past three years and during the study period. These low water levels were amongst the lowest on record and it is likely that the public would attribute any adverse effect recorded in the future to the abstraction scheme, whether this were true or not. These negative perceptions of the desirability and acceptability of the proposed scheme were strongly linked to potential adverse affects on the tourism industry along the Okavango River and in the Okavango Delta, with possible adverse economic effects on local residents.     

Salt-water coupling in leaky epithelia

Summary The theory of quasi-isotonic transport by cellular osmosis (the standing-gradient theory) has been challenged on the grounds that the osmotic permeabilities of the mucosal and interspace membranes are too low; if they were as high as the theory requires then the osmotic permeability of the whole epithelium would be 2–3 orders of magnitude higher than observed. This objection has basically been accepted for it is now claimed that these enormous permeabilities do exist, but are masked by unstirred-layer effects; I show that this is incorrect because unstirredlayer corrections are small and that the situation has not changed since 1975.The view that the route of fluid transport is junctional is replacing the cellular theory, and trans-junctional water flows seem to account for major fractions of the flow in various epithelia. I argue on grounds of general theory that these are unlikely to be osmotic flows because the junctional pores cannot satisfy both the osmotic and diffusive properties required of them, but the basic osmotic theory is also rather vague here.Non-osmotic theories, if junctional flow is accepted, must be either electro-kinetic or peristaltic.     

Effects of exogenous amines on mammalian cells, with particular reference to membrane flow.

We have reviewed the evidence that amines accumulate in intracellular vesicles of low pH, such as lysosomes and endosomes. There is consequent elevation of intravesicular pH, and inhibition of receptor-ligand dissociation often results from this pH change. We have argued that the capacity for fusion of such vesicles is also reduced by the high pH. We suggest that the variety of effects of amines on membrane flow and macromolecular transport we describe are at least partly due to such reduced fusion (Figs. 1 and 2). We propose that an internal low pH may facilitate heterologous vesicle-vesicle and vesicle-plasma membrane fusion. There is some evidence that clathrin can accelerate phospholipid vesicle fusion in vitro at low pH (Blumenthal et al., 1983) but no direct evidence on the role of intravesicular pH. This idea is consistent not only with the preceding discussion, but also with the fact that the intracellular membrane-bound compartments least involved in fusion events (e.g. mitochondria) are of neutral or alkaline internal pH. Membrane fusion is certainly required for the formation of vesicles at the periphery of the Golgi apparatus, and possibly earlier in the transport and processing of biosynthetic products in the Golgi (Bergeron et al., 1982). Thus the accumulation of amines in the Golgi may be responsible for several effects on the flow of macromolecules along their translocation pathways. The status of the plasma membrane in this view is complex. It might be argued that the pH dictating the fusion step in endocytosis is that of the extracellular fluid, in which case the inhibitory effects of amines on this process are not explained. However, the rapidity of acidification of the newly formed endocytic vesicles allows the possibility that plasma membrane invaginations might temporarily sequester areas which are of lower pH than that of the bulk extracellular fluid even before fusion, since the proton pumping enzyme(s) are probably present on the plasma membrane. Were this the case, then an acid pH could again be a factor determining membrane fusion at the plasma membrane. The inhibition of endocytosis by weak bases thus may again reflect elevation of pH in a sequestered compartment. From the data on the dependence of response on the concentration of amines, we anticipate that most responses involving membrane flow will be biphasic, with inhibitory effects at low amine concentration, giving way to stimulatory ones at higher concentrations. We suggest that the reported dichotomy between different amines in intracellular membrane fusion systems (D'Arcy Hart, 1982) may result from this concentration dependence.(ABSTRACT TRUNCATED AT 400 WORDS)     

贡嘎山暗针叶林土壤优先流形成因素的初步研究

该研究以长江上游贡嘎山暗针叶林生态系统的降雨过程、地被物层、根系层及土壤层的生长发育特点和水分运动状况为基础,利用自制实验仪器,在研究区域开展室内土柱实验,与野外实地示踪影像分析及树种根系调查相结合,针对研究区域土壤包气带根系层中水分快速运动的优先流形成的内外影响因子展开研究工作。研究结果表明研究区域土壤松散和多孔,土壤的孔隙度较大,大部分降雨为低强度、低雨量级和长历时,并具有较厚的地被物层和丰富的根系层,这些诱发因素存在,使研究区域——贡嘎山高山生态系统具有优先流形成的条件,降雨不会对土壤造成击溅作用,水分运移沿着土壤孔隙或植物根孔等处开辟优先路径,在地被物层及土壤层形成一个水流通道,随着长历时的降雨的继续,水分及其所携带的溶质继续沿着此路径向下运移。     

黄土高原景观格局与水土流失关系研究

采用DCCA排序法对黄土高原腹地泾河流域12个子流域的景观格局与流域水土流失关系进行了定量分析.结果表明,DCCA排序的前4轴分别与农业用地比率、景观多样性指数、森林比率显著相关.各子流域的水土流失特征具有明显的梯度变异.在森林比率占65%的三水河子流域,景观相对简单、多样性低,流域年径流量大、输沙小、含沙量低,径流相对稳定;随着森林比率减小,农业用地比率增大,景观多样性升高,产流系数增高,径流深度、输沙量和含沙量增大;在森林比率很低、农业用地53.41%的洪河子流域,景观格局复杂、多样性较高,河流含沙量高、输沙率大,月输沙和径流变异极大;在农业用地比率减小,其他景观类型比率增大,景观相对简单的环江上、下游子流域,输沙量和含沙量减小,但输沙和径流的年际变化极大.排序分析结果较清晰地解释了黄土高原典型地区水土流失特征沿景观梯度的变化规律.     

黄河口邻近海域生态系统能量流动与三疣梭子蟹增殖容量估算

增殖放流是渔业资源养护的重要手段, 生态系统与放流种类能流格局的变化研究,是进行增殖容量评估的研究基础.根据2012和2013年黄河口邻近海域的资源调查数据,构建了黄河口邻近海域6、8、10月的Ecopath模型,比较分析了3个月份该海域生态系统能量流动的变化,初步评估了三疣梭子蟹的增殖容量.结果表明： 黄河口邻近海域生态系统的能量流动主要在营养级I～III之间进行,营养级IV以及以上的能量流动较小.6月第I营养级整合系统流动的比例最高,8月最低.第II营养级整合系统流动的比例8月最高,6月最低.三疣梭子蟹相对能量流动和绝对能量流动均是第III营养级最高,三疣梭子蟹的营养级3月平均为3.28.黄河口邻近海域生态系统有较高的剩余生产量,6月最高、8月最低,系统的总初级生产量/总呼吸(TPP/TR) 3个月份分别为5.49、2.47、3.01,总初级生产量/总生物量(TPP/B)分别为47.61、33.30、29.78,同时具有较低的循环指数(FCI：0.03～0.06),黄河口邻近海域生态系统处于脆弱的不稳定期.系统的能量转换效率为7.3%～11.5%;渔获物的平均营养级8月和10月有所下降,3个月份分别为3.23、2.97和2.82;总捕捞效率8月最高,6月最低.在黄河口邻近海域8月Ecopath模型基础上,初步评估三疣梭子蟹的增殖容量为1.5115 t·km^-2.     

Evaluation of glucose transport and its regulation by insulin in human monocytes using flow cytometry.

BACKGROUND: We investigated the effects of insulin on glucose transport in human monocytes using flow cytometry, a method with several advantages over previously used techniques. We hypothesized that monocytes could be used as tools to study insulin action at the cellular level and facilitate the investigation of mechanisms that lead to insulin resistance. METHODS: Blood was withdrawn from 38 healthy subjects. The expression of glucose transporter (GLUT) isoforms in plasma membrane and the rates of glucose transport were determined with and without insulin (10 to 1,000 mU/L). Anti-CD14 phycoerythrin monoclonal antibody was used for monocyte gating. GLUT isoforms were determined after staining cells with specific antisera to GLUT1, GLUT3, and GLUT4. Glucose transport was monitored with 6-[N-(7-nitrobenz-2-oxa-1,3-diazol-4-yl)amino]-6-deoxyglucose (NBDG). RESULTS: Insulin increased the uptake of NBDG (median effective dose 20 mU/L) and the expression of GLUT3 and GLUT4 isoforms in the plasma membrane (median effective doses 20 and 35 mU/L, respectively) but had no effect on GLUT1. Maximal effects were always reached at 100 mU/L of insulin. CONCLUSIONS: Monocytes may be a valid model system to study the effects of insulin on glucose transport. Further, flow cytometry is suitable for this investigation and can be used as an alternative to radiotracer methods.     

Inhibition of energy-transducing functions of chloroplasts by spegazzinine.

The effects of spegazzinine, a dihydroindole alkaloid, on various energy-transducing functions of chloroplasts were studied. The following observations were made, (i) Spegazzinine inhibited both cyclic and noncyclic photophosphorylation in isolated spinach chloroplast. The I₅₀ value was about 80 μm. Over a concentration range which gave marked inhibition of ÀTP synthesis, there was no effect on basal or uncoupled electron flow or light-induced proton accumulation by isolated thylakoids, while the fraction of electron transport stimulated by coupled phosphorylation was reduced to the basal level by spegazzinine. (ii) The regulatory effect of low concentrations of ATP on proton movements and electron transport was diminished by the alkaloid, (iii) Spegazzinine also inhibited with similar efficiency the ATPase activities of membrane-bound coupling factor 1 (CF₁) and of purified CF₁. One mole of spegazzinine per mole of CF₁ seemed to be required to inhibit the ATPase activity, (iv) The allosteric effect of ADP on ATPase activity was not affected by spegazzinine. (v) On the basis of these results it is concluded that spegazzinine acts as an energy transfer inhibitor of hotophosphorylation and that its site of action may be at or near the catalytic site of ATPase.     

Effect of non-Newtonian and pulsatile blood flow on mass transport in the human aorta

To investigate the effects of both non-Newtonian behavior and the pulsation of blood flow on the distributions of luminal surface LDL concentration and oxygen flux along the wall of the human aorta, we numerically compared a non-Newtonian model with the Newtonian one under both steady flow and in vivo pulsatile flow conditions using a human aorta model constructed from MRI images. The results showed that under steady flow conditions, although the shear thinning non-Newtonian nature of blood could elevate wall shear stress (WSS) in most regions of the aorta, especially areas with low WSS, it had little effect on luminal surface LDL concentration (c(w)) in most regions of the aorta. Nevertheless, it could significantly enhance c(w) in areas with high luminal surface LDL concentration through the shear dependent diffusivity of LDLs. For oxygen transport, the shear thinning non-Newtonian nature of blood could slightly reduce oxygen flux in most regions of the aorta, but this effect became much more apparent in areas with already low oxygen flux. The pulsation of blood flow could significantly reduce c(w) and enhance oxygen flux in these disturbed places. In most other regions of the aorta, the oxygen flux was also significantly higher than that for the steady flow simulation. In conclusion, the shear shining non-Newtonian nature of blood has little effect on LDL and oxygen transport in most regions of the aorta, but in the atherogenic-prone areas where luminal surface LDL concentration is high and oxygen flux is low, its effect is apparent. Similar is for the effect of pulsatile flow on the transport of LDLs. But, the pulsation of blood flow can apparently affect oxygen flux in the aorta, especially in areas with low oxygen flux.     

On transport of suspended particulates in tube flow.

Blood cells suspended in shear flows exhibit much larger dispersive motions than those predicted by the Stokes-Einstein formula for Brownian diffusion. The lateral migration and the erratic motions of the 8 microns red blood cells (RBC) is thought to be analogous to a diffusive process. It is shown that the often cited convective-diffusion theory may not be an adequate model for describing the transverse migration of suspended cells in blood flow. A comprehensive review of both the classical theory and of contemporary work in particle transport is presented, with particular emphasis on low Reynolds number tube flows. The mechanisms of Taylor dispersion, the effects of Brownian perturbations on translational and rotational motions of the suspended particles in shear fields, and the influence of integratable and chaotic advections, are individually examined. The classical experiment by Segre and Silberberg (1962) lead us to believe that particle hydrodynamics may play an important role in transverse migrations. In this light, we have further examined the hydrodynamic aspects of the so-called "tubular pinch" effect, the lateral migration of rigid spheres. We have also discussed the transverse motions of liquid drops, and the reversibility of the organization of suspensions in transport. The convective accelerations in the entrance region of a tube can produce relative velocities between fluid medium and various type of particulates if there is a difference in density. The deformable RBC, an "active-type" particle, can provide feedback to the flow from both mass and momentum considerations; the more rigid platelet, a "passive-type" particle, will experience a much smaller relative velocity as compared to the RBC. We may expect that particles of different densities are transported to different equilibrium annular positions before entering the fully developed flow region. The erratic, lateral movement of suspended particulates in steady laminar tube flow can be described by the usual Lagrangian coordinates.