淹水条件下添加有机物料对蔬菜地土壤硝态氮及氮素气体排放的影响

蔬菜地大量施用氮肥可以引起土壤硝态氮积累,导致土壤退化,快速消除土壤积累的硝态氮,可以提高蔬菜地土壤质量,延长其使用时间.在硝态氮(360 mg N·kg^-1)积累的蔬菜地土壤中,分别加入0、2500、5000和7500 kg C·hm^-2黑麦草(记为CK、C₂₅₀₀、C₅₀₀₀和C₇₅₀₀),淹水条件下,30 ℃恒温室内培养240 h,研究土壤硝态氮含量及氮素气体排放量变化.结果表明：培养结束时,CK处理中土壤硝态氮含量高达310 mg N·kg^-1,添加黑麦草能有效地消除土壤中积累的硝态氮,C₂₅₀₀、C₅₀₀₀和C₇₅₀₀处理中土壤硝态氮含量降低至10 mg N·kg^-1以下需要的时间分别为240、48和24 h.添加黑麦草显著提高了土壤pH,降低了土壤电导率,其变化幅度随黑麦草添加量的增加而增大.添加黑麦草处理的土壤N₂O和N₂累积排放量为270～378 mg N·kg^-1,N₂O/N₂为0.6～1.5.淹水条件下添加黑麦草可快速消除蔬菜地土壤积累的硝态氮,但应充分重视N₂O在这一过程中的大量排放.     

Unique oxidative mechanisms for the reactive nitrogen oxide species, nitroxyl anion

The nitroxyl anion (NO-) is a highly reactive molecule that may be involved in pathophysiological actions associated with increased formation of reactive nitrogen oxide species. Angeli's salt (Na2N2O3; AS) is a NO- donor that has been shown to exert marked cytotoxicity. However, its decomposition intermediates have not been well characterized. In this study, the chemical reactivity of AS was examined and compared with that of peroxynitrite (ONOO-) and NO/N2O3. Under aerobic conditions, AS and ONOO- exhibited similar and considerably higher affinities for dihydrorhodamine (DHR) than NO/N2O3. Quenching of DHR oxidation by azide and nitrosation of diaminonaphthalene were exclusively observed with NO/N2O3. Additional comparison of ONOO- and AS chemistry demonstrated that ONOO- was a far more potent one-electron oxidant and nitrating agent of hydroxyphenylacetic acid than was AS. However, AS was more effective at hydroxylating benzoic acid than was ONOO-. Taken together, these data indicate that neither NO/N2O3 nor ONOO- is an intermediate of AS decomposition. Evaluation of the stoichiometry of AS decomposition and O2 consumption revealed a 1:1 molar ratio. Indeed, oxidation of DHR mediated by AS proved to be oxygen-dependent. Analysis of the end products of AS decomposition demonstrated formation of NO2- and NO3- in approximately stoichiometric ratios. Several mechanisms are proposed for O2 adduct formation followed by decomposition to NO3- or by oxidation of an HN2O3- molecule to form NO2-. Given that the cytotoxicity of AS is far greater than that of either NO/N2O3 or NO + O2, this study provides important new insights into the implications of the potential endogenous formation of NO- under inflammatory conditions in vivo.     

Production of NO, N2O and N2 by extracted soil bacteria, regulation by NO2(-) and O2 concentrations.

The oxygen control of denitrification and its emission of NO/N2O/N2 was investigated by incubation of Nycodenz-extracted soil bacteria in an incubation robot which monitors O2, NO, N2O and N2 concentrations (in He+O2 atmosphere). Two consecutive incubations were undertaken to determine (1) the regulation of denitrification by O2 and NO2(-) during respiratory O2 depletion and (2) the effects of re-exposure to O2 of cultures with fully expressed denitrification proteome. Early denitrification was only detected (as NO and N2O) at 相似文献   

Level of nitric oxide in hypertensive patients scheduled on general anaesthesia

In this prospective study we have analysed the level of nitric oxide in hypertensive patients scheduled for general anaesthesia. In the study were included thirty-four patients with chronicle inflammatory disease of the middle ear who have undergone surgical treatment at the Clinic for Ear, Nose and Throat Surgery. The aim of our study was to determine the plasma level of nitric oxide (NO) and its effects on the circulatory system in hypertensive patients during the general anaesthesia maintained with inhalation of oxygen and nitrous oxide (O2/N2O) mixture. Patients were divided in two groups. During the maintenance of general anaesthesia the patients from the first group were ventilated with O2/N2O, while patients from the second group were ventilated with oxygen and air (O2/air) mixture. The other principles during the general anaesthesia were equal for both groups. For determination of the NO plasma levels we have used the enzymatic method according to Conrad et al., 1993. Our results showed that there is a statistically significant difference of NO plasma level between the two groups. The level of NO was higher in the first group (ventilated with O2/N2O) compared to the second group (ventilated with O/air). The mean arterial pressure and systemic vascular resistance were significantly decreased in the first group, as well. Our results suggest that nitrous oxide (N2O) most probably plays the role of NO donor in hypertensive patients during the maintenance of the general anaesthesia with N2O/O2 mixture.     

Determination of key metabolites during biodegradation of hexahydro-1,3,5-trinitro-1,3,5-triazine with Rhodococcus sp. strain DN22.

Rhodococcus sp. strain DN22 can convert hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) to nitrite, but information on degradation products or the fate of carbon is not known. The present study describes aerobic biodegradation of RDX (175 microM) when used as an N source for strain DN22. RDX was converted to nitrite (NO(2)(-)) (30%), nitrous oxide (N(2)O) (3.2%), ammonia (10%), and formaldehyde (HCHO) (27%), which later converted to carbon dioxide. In experiments with ring-labeled [(15)N]-RDX, gas chromatographic/mass spectrophotometric (GC/MS) analysis revealed N(2)O with two molecular mass ions: one at 44 Da, corresponding to (14)N(14)NO, and the second at 45 Da, corresponding to (15)N(14)NO. The nonlabeled N(2)O could be formed only from -NO(2), whereas the (15)N-labeled one was presumed to originate from a nitramine group ((15)N-(14)NO(2)) in RDX. Liquid chromatographic (LC)-MS electrospray analyses indicated the formation of a dead end product with a deprotonated molecular mass ion [M-H] at 118 Da. High-resolution MS indicated a molecular formula of C(2)H(5)N(3)O(3). When the experiment was repeated with ring-labeled [(15)N]-RDX, the [M-H] appeared at 120 Da, indicating that two of the three N atoms in the metabolite originated from the ring in RDX. When [U-(14)C]-RDX was used in the experiment, 64% of the original radioactivity in RDX incorporated into the metabolite with a molecular weight (MW) of 119 (high-pressure LC/radioactivity) and 30% in (14)CO(2) (mineralization) after 4 days of incubation, suggesting that one of the carbon atoms in RDX was converted to CO(2) and the other two were incorporated in the ring cleavage product with an MW of 119. Based on the above stoichiometry, we propose a degradation pathway for RDX based on initial denitration followed by ring cleavage to formaldehyde and the dead end product with an MW of 119.     

Denitrification, dissimilatory reduction of nitrate to ammonium, and nitrification in a bioturbated estuarine sediment as measured with N and microsensor techniques

Nitrogen and oxygen transformations were studied in a bioturbated (reworked by animals) estuarine sediment (Norsminde Fjord, Denmark) by using a combination of N isotope (NO(3)), specific inhibitor (C(2)H(2)), and microsensor (N(2)O and O(2)) techniques in a continuous-flow core system. The estuarine water was NO(3) rich (125 to 600 muM), and NO(3) was consistently taken up by the sediment on the four occasions studied. Total NO(3) uptake (3.6 to 34.0 mmol of N m day) corresponded closely to N(2) production (denitrification) during the experimental steady state, which indicated that dissimilatory, as well as assimilatory, NO(3) reduction to NH(4) was insignificant. When C(2)H(2) was applied in the flow system, denitrification measured as N(2)O production was often less (58 to 100%) than the NO(3) uptake because of incomplete inhibition of N(2)O reduction. The NO(3) formed by nitrification and not immediately denitrified but released to the overlying water, uncoupled nitrification, was calculated both from NO(3) dilution and from changes in NO(3) uptake before and after C(2)H(2) addition. These two approaches gave similar results, with rates ranging between 0 and 8.1 mmol of N m day on the four occasions. Attempts to measure total nitrification activity by the difference between NH(4) fluxes before and after C(2)H(2) addition failed because of non-steady-state NH(4) fluxes. The vertical distribution of denitrification and oxygen consumption was studied by use of N(2)O and O(2) microelectrodes. The N(2)O profiles measured during the experimental steady state were often irregularly shaped, and the buildup of N(2)O after C(2)H(2) was added was much too fast to be described by a simple diffusion model. Only bioturbation by a dense population of infauna could explain these observations. This was corroborated by the relationship between diffusive and total fluxes, which showed that only 19 to 36 and 29 to 62% of the total O(2) uptake and denitrification, respectively, were due to diffusion-reaction processes at the regular sediment surface, excluding animal burrows.     

A comparison of NO and N2O production by the autotrophic nitrifier Nitrosomonas europaea and the heterotrophic nitrifier Alcaligenes faecalis.

Soil microorganisms are important sources of the nitrogen trace gases NO and N2O for the atmosphere. Present evidence suggests that autotrophic nitrifiers such as Nitrosomonas europaea are the primary producers of NO and N2O in aerobic soils, whereas denitrifiers such as Pseudomonas spp. or Alcaligenes spp. are responsible for most of the NO and N2O emissions from anaerobic soils. It has been shown that Alcaligenes faecalis, a bacterium common in both soil and water, is capable of concomitant heterotrophic nitrification and denitrification. This study was undertaken to determine whether heterotrophic nitrification might be as important a source of NO and N2O as autotrophic nitrification. We compared the responses of N. europaea and A. faecalis to changes in partial O2 pressure (pO2) and to the presence of typical nitrification inhibitors. Maximal production of NO and N2O occurred at low pO2 values in cultures of both N. europaea (pO2, 0.3 kPa) and A. faecalis (pO2, 2 to 4 kPa). With N. europaea most of the NH4+ oxidized was converted to NO2-, with NO and N2O accounting for 2.6 and 1% of the end product, respectively. With A. faecalis maximal production of NO occurred at a pO2 of 2 kPa, and maximal production of N2O occurred at a pO2 of 4 kPa. At these low pO2 values there was net nitrite consumption. Aerobically, A. faecalis produced approximately the same amount of NO but 10-fold more N2O per cell than N. europaea did. Typical nitrification inhibitors were far less effective for reducing emissions of NO and N2O by A. faecalis than for reducing emissions of NO and N2O by N. europaea.(ABSTRACT TRUNCATED AT 250 WORDS)     

Decreased N2O reduction by low soil pH causes high N2O emissions in a riparian ecosystem

Quantification of harmful nitrous oxide (N(2)O) emissions from soils is essential for mitigation measures. An important N(2)O producing and reducing process in soils is denitrification, which shows deceased rates at low pH. No clear relationship between N(2)O emissions and soil pH has yet been established because also the relative contribution of N(2)O as the denitrification end product decreases with pH. Our aim was to show the net effect of soil pH on N(2)O production and emission. Therefore, experiments were designed to investigate the effects of pH on NO(3)(-) reduction, N(2)O production and reduction and N(2) production in incubations with pH values set between 4 and 7. Furthermore, field measurements of soil pH and N(2)O emissions were carried out. In incubations, NO(3)(-) reduction and N(2) production rates increased with pH and net N(2)O production rate was highest at pH 5. N(2)O reduction to N(2) was halted until NO(3)(-) was depleted at low pH values, resulting in a built up of N(2)O. As a consequence, N(2)O:N(2) production ratio decreased exponentially with pH. N(2)O reduction appeared therefore more important than N(2)O production in explaining net N(2)O production rates. In the field, a negative exponential relationship for soil pH against N(2)O emissions was observed. Soil pH could therefore be used as a predictive tool for average N(2)O emissions in the studied ecosystem. The occurrence of low pH spots may explain N(2)O emission hotspot occurrence. Future studies should focus on the mechanism behind small scale soil pH variability and the effect of manipulating the pH of soils.     

Nitrate and nitrite microgradients in barley rhizosphere as detected by a highly sensitive denitrification bioassay.

A highly sensitive denitrification bioassay was developed for detection of NO3- and NO2- in rhizosphere soil samples. Denitrifying Pseudomonas aeruginosa ON12 was grown anaerobically in citrate (30 mM) minimal medium with KClO3 (10 mM) and NaNO2 (3 mM), which gave cells capable of NO2- reduction to N2O but incapable of NO3- reduction to NO2-. Growth on citrate minimal medium further resulted in the absence of N2O reduction. When added to small soil samples in O2-free vials, such cells could be used to convert the indigenous NO2- pool to N2O, which was subsequently quantified by gas chromatography. Cells grown in KClO3-free citrate medium with 10 mM NaNO3 as the electron acceptor were capable of reducing both NO3- and NO2-, and these cells could subsequently be added to the sample to convert the indigenous NO3- pool to N2O. Concentrations of both NO3- and NO2- were thus determined as N2O, with a detection limit of approximately 10 pmol of N. The bioassay could be used to determine NO3- and NO2- pools in 10-mg soil samples taken along a microgradient in the rhizosphere of field-grown barley plants. At both low (10%, wt/wt) and high (18%, wt/wt) water content, relatively high levels of NO2- were found in the rhizosphere compared with bulk soil. Under dry conditions, NO3- was also more abundant in the rhizosphere than in the bulk soil, whereas such a difference was not observed at the high water content. The roles of plant metabolism and bacterial nitrification and denitrification processes for NO3- and NO2- availability in the rhizosphere are discussed.     

Catalysis of dehydrogenation of 4-trans-(N,N-dimethylamino)cinnamaldehyde by aldehyde dehydrogenase

4-trans-(N,N-dimethylamino)cinnamaldehyde (DACA) is a chromophoric and fluorogenic substrate of aldehyde dehydrogenase. Fluorescence of DACA is enhanced by binding to aldehyde dehydrogenase in the absence of catalysis both in the presence and absence of the coenzyme analogue 5'AMP. DACA binds to aldehyde dehydrogenase with a dissociation constant of 1-3 microM and stoichiometry of 2 mol mol(-1) enzyme. Incorporation of DACA during catalysis was also investigated and found to be 2 mol DACA mol(-1) enzyme. Effect of pH on the stoichiometry of DACA incorporation during catalysis has shown that DACA incorporation remained constant at 2 mol DACA mol(-1) enzyme, despite a 74-fold velocity enhancement between pH 5.0 and 9.0. Increase of pH increased decomposition of enzyme-acyl intermediate without affecting the rate-limiting step of the reaction. At pH 7.0 the pH stimulated velocity enhancement was 10-fold over that at pH 5.0; further velocity enhancement (11.5-fold that of pH 7.0) was achieved by 150 microM Mg(2+) ions. The velocity at pH 7.0 with Mg(2+) exceeded that of pH 9.0, and that at maximal pH stimulation at pH 9.5. It was observed that level of intermediate decreased to about 1 mol mol(-1) enzyme, indicating that Mg(2+) ions increased the rate of decomposition of the enzyme-acyl intermediate and shifted the rate-limiting step of the reaction to another step in the reaction sequence.     

Nitrate and nitrite microgradients in barley rhizosphere as detected by a highly sensitive denitrification bioassay.

A highly sensitive denitrification bioassay was developed for detection of NO3- and NO2- in rhizosphere soil samples. Denitrifying Pseudomonas aeruginosa ON12 was grown anaerobically in citrate (30 mM) minimal medium with KClO3 (10 mM) and NaNO2 (3 mM), which gave cells capable of NO2- reduction to N2O but incapable of NO3- reduction to NO2-. Growth on citrate minimal medium further resulted in the absence of N2O reduction. When added to small soil samples in O2-free vials, such cells could be used to convert the indigenous NO2- pool to N2O, which was subsequently quantified by gas chromatography. Cells grown in KClO3-free citrate medium with 10 mM NaNO3 as the electron acceptor were capable of reducing both NO3- and NO2-, and these cells could subsequently be added to the sample to convert the indigenous NO3- pool to N2O. Concentrations of both NO3- and NO2- were thus determined as N2O, with a detection limit of approximately 10 pmol of N. The bioassay could be used to determine NO3- and NO2- pools in 10-mg soil samples taken along a microgradient in the rhizosphere of field-grown barley plants. At both low (10%, wt/wt) and high (18%, wt/wt) water content, relatively high levels of NO2- were found in the rhizosphere compared with bulk soil. Under dry conditions, NO3- was also more abundant in the rhizosphere than in the bulk soil, whereas such a difference was not observed at the high water content. The roles of plant metabolism and bacterial nitrification and denitrification processes for NO3- and NO2- availability in the rhizosphere are discussed.     

Is N2O3 the main nitrosating intermediate in aerated nitric oxide (NO) solutions in vivo? If so,where, when,and which one?

The widespread opinion that N(2)O(3) as a product of NO oxidation is the only nitros(yl)ating agent under aerobic conditions is based on experiments in homogeneous buffered water solutions. In vivo NO is oxidized in heterogeneous media and this opinion is not correct. The equilibrium in the system being dependent on temperature and DeltaG((sol)) for NO, NO(2), isomers of both N(2)O(3), and N(2)O(4). For polar solvents including water, DeltaG((sol)) for N(2)O(3) is high enough, and a stationary concentration of N(2)O(3) in the mixture with other oxides is sufficient to guarantee the hydrolysis of N(2)O(3) to nitrite. In heterogeneous media, the mixture contains solvates NO(2(sol)), N(2)O(3(sol)), and N(2)O(4(sol)) at stationary nonequilibrium concentrations. As far as DeltaG((sol)) is decreased in heterogeneous mixtures with low polar solvents and/or at increased temperatures, the equilibrium in such a system shifts to NO(2). Although NO(2) is a reactive free radical, it almost does not react with water. In contrast, the reaction with most functional protein groups efficiently proceeds by a radical type with the formation of nitrite and new radicals (X) further stabilized in various forms. Therefore, the ratio of the nitrosylated and nitrated products yields depends on actual concentrations of all NO(x).     

Binding and incorporation of 4-trans-(N,N-dimethylamino) cinnamaldehyde by aldehyde dehydrogenase

4-trans-(N,N-Dimethylamino)cinnamaldehyde (DACA) is a chromophoric substrate of aldehyde dehydrogenase (EC 1.2.1.3) whose fate can be followed during catalysis. During this investigation we found that DACA also fluoresces and that this fluorescence is enhanced and blue-shifted upon binding to aldehyde dehydrogenase. Binding of DACA to aldehyde dehydrogenase also occurs in the absence of coenzyme. Benzaldehyde (a substrate), acetophenone (a substrate-competitive inhibitor), and the substrate-competitive affinity reagent bromoaceto-phenone interfere with DACA binding. Thus, DACA binds to the active site and can be employed for titration of active aldehyde dehydrogenase. Both E1 and E2 isozymes, which are homotetramers, bind DACA with dissociation constants of 1–4 M with a stoichiometry of 2 mol DACA/mol enzyme. The stoichiometry of enzyme–acyl intermediate was also found to be 2 mol DACA/mol enzyme for both E1 and E2 isozymes. Thus, both enzymes appear to have only two substrate-binding sites which participate in catalysis. The level of enzyme–acyl intermediate remained constant at different pH values, showing that enhancement of velocity with pH was not due to altered DACA–enzyme levels. When the reaction velocity was increased even further by using 150 M Mg²⁺ the intermediate level was decreased, suggesting that both increased pH and Mg²⁺ promote decomposition of the DACA–enzyme intermediate. Titration with DACA permits study of aldehyde substrate catalysis before central complex interconversion.     

Sub-Parts-Per-Billion Nitrate Method: Use of an N(2)O-Producing Denitrifier to Convert NO(3) or NO(3) to N(2)O

A more sensitive analytical method for NO(3) was developed based on the conversion of NO(3) to N(2)O by a denitrifier that could not reduce N(2)O further. The improved detectability resulted from the high sensitivity of the Ni electron capture gas chromatographic detector for N(2)O and the purification of the nitrogen afforded by the transformation of the N to a gaseous product with a low atmospheric background. The selected denitrifier quantitatively converted NO(3) to N(2)O within 10 min. The optimum measurement range was from 0.5 to 50 ppb (50 mug/liter) of NO(3) N, and the detection limit was 0.2 ppb of N. The values measured by the denitrifier method compared well with those measured by the high-pressure liquid chromatographic UV method above 2 ppb of N, which is the detection limit of the latter method. It should be possible to analyze all types of samples for nitrate, except those with inhibiting substances, by this method. To illustrate the use of the denitrifier method, NO(3) concentrations of <2 ppb of NO(3) N were measured in distilled and deionized purified water samples and in anaerobic lake water samples, but were not detected at the surface of the sediment. The denitrifier method was also used to measure the atom% of N in NO(3). This method avoids the incomplete reduction and contamination of the NO(3) -N by the NH(4) and N(2) pools which can occur by the conventional method of NO(3) analysis. N(2)O-producing denitrifier strains were also used to measure the apparent K(m) values for NO(3) use by these organisms. Analysis of N(2)O production by use of a progress curve yielded K(m) values of 1.7 and 1.8 muM NO(3) for the two denitrifier strains studied.     

Comparison of control of Listeria by nitric oxide redox chemistry from murine macrophages and NO donors: insights into listeriocidal activity of oxidative and nitrosative stress

The physiological function of nitric oxide (NO) in the defense against pathogens is multifaceted. The exact chemistry by which NO combats intracellular pathogens such as Listeria monocytogenes is yet unresolved. We examined the effects of NO exposure, either delivered by NO donors or generated in situ within ANA-1 murine macrophages, on L. monocytogenes growth. Production of NO by the two NONOate compounds PAPA/NO (NH2(C3H6)(N[N(O)NO]C3H7) and DEA/NO (Na(C2H5)2N[N(O)NO]) resulted in L. monocytogenes cytostasis with minimal cytotoxicity. Reactive oxygen species generated from xanthine oxidase/hypoxanthine were neither bactericidal nor cytostatic and did not alter the action of NO. L. monocytogenes growth was also suppressed upon internalization into ANA-1 murine macrophages primed with interferon-gamma (INF-gamma) + tumor necrosis factor-alpha (TNF-alpha or INF-gamma + lipid polysaccharide (LPS). Growth suppression correlated with nitrite formation and nitrosation of 2,3-diaminonaphthalene elicited by stimulated murine macrophages. This nitrosative chemistry was not dependent upon nor mediated by interaction with reactive oxygen species (ROS), but resulted solely from NO and intermediates related to nitrosative stress. The role of nitrosation in controlling L. monocytogenes was further examined by monitoring the effects of exposure to NO on an important virulence factor, Listeriolysin O, which was inhibited under nitrosative conditions. These results suggest that nitrosative stress mediated by macrophages is an important component of the immunological arsenal in controlling L. monocytogenes infections.     

Dissimilatory Reduction of NO(2) to NH(4) and N(2)O by a Soil Citrobacter sp

Dissimilatory reduction of NO(2) to N(2)O and NH(4) by a soil Citrobacter sp. was studied in an attempt to elucidate the physiological and ecological significance of N(2)O production by this mechanism. In batch cultures with defined media, NO(2) reduction to NH(4) was favored by high glucose and low NO(3) concentrations. Nitrous oxide production was greatest at high glucose and intermediate NO(3) concentrations. With succinate as the energy source, little or no NO(2) was reduced to NH(4) but N(2)O was produced. Resting cell suspensions reduced NO(2) simultaneously to N(2)O and free extracellular NH(4). Chloramphenicol prevented the induction of N(2)O-producing activity. The K(m) for NO(2) reduction to N(2)O was estimated to be 0.9 mM NO(2), yet the apparent K(m) for overall NO(2) reduction was considerably lower, no greater than 0.04 mM NO(2). Activities for N(2)O and NH(4) production increased markedly after depletion of NO(3) from the media. Amendment with NO(3) inhibited N(2)O and NH(4) production by molybdate-grown cells but not by tungstate-grown cells. Sulfite inhibited production of NH(4) but not of N(2)O. In a related experiment, three Escherichia coli mutants lacking NADH-dependent nitrite reductase produced N(2)O at rates equal to the wild type. These observations suggest that N(2)O is produced enzymatically but not by the same enzyme system responsible for dissimilatory reduction of NO(2) to NH(4).     

Endocardial endothelium in the avascular frog heart: role for diffusion of NO in control of cardiac O2 consumption

We investigated the role of nitric oxide (NO) in the control of myocardial O(2) consumption in the hearts of female Xenopus frogs, which lack a coronary vascular endothelium and in which the endocardial endothelium is the only source of NO to regulate cardiac myocyte function. Hence, frogs are an ideal model in which to explore the role of diffusion of NO from the endocardial endothelium (EE) without vascular endothelial or cardiac cell NO production. In Xenopus hearts we examined the regulation of cardiac O(2) consumption in vitro at 25 degrees C and 37 degrees C. The NO-mediated control of O(2) consumption by bradykinin or carbachol was significantly (P < 0.05) lower at 25 degrees C (79 +/- 13 or 73 +/- 11 nmol/min) than at 37 degrees C (159 +/- 26 or 201 +/- 13 nmol/min). The response to the NO donor S-nitroso-N-acetyl penicillamine was also markedly lower at 25 degrees C (90 +/- 8 nmol/min) compared with 37 degrees C (218 +/- 15 nmol/min). When Triton X-100 was perfused into hearts, the inhibition of myocardial O(2) consumption by bradykinin (18 +/- 2 nmol/min) or carbachol (29 +/- 4 nmol/min) was abolished. Hematoxylin and eosin slides of Triton X-100-perfused heart tissue confirmed the absence of the EE. Although endothelial NO synthase protein levels were decreased to a variable degree in the Triton X-100-perfused heart, NO(2) production (indicating eNOS activity) decreased by >80%. It appears that the EE of the frog heart is the sole source of NO to regulate myocyte O(2) consumption. When these cells are removed, the ability of NO to regulate O(2) consumption is severely limited. Thus our results suggest that the EE produces enough NO, which diffuses from the EE to cardiac myocytes, to regulate myocardial O(2) consumption. Because of the close proximity of the EE to underlying myocytes, NO can diffuse over a distance and act as a messenger between the EE and the rest of the heart to control mitochondrial function and O(2) consumption.     

The reduction of Fusobacterium nucleatum in mice is irrelevant to the nitric oxide induced by iNOS

Previously we reported that mice infected recurrently with live Fusobacterim nucleatum (Fn) synthesize a significant amount of NO between 12 hr and 24 hr after the Fn injection. We now investigated whether the NO has the capability of killing Fn, a gram-negative rod periodontal pathogen. The mice were divided into three groups: treated with live bacteria (LB), treated with heat-killed bacteria (HKB) and untreated: normal (N). The Fn reduction, NO production and cell number after Fn injection were then compared in these mice. In the LB group, no Fn was detected at 6 hr, whereas it was still detected in the HKB and N groups at 24 hr as assessed by both colony counts and PCR assays. A significant amount of NO was synthesized in the LB group at 24 hr after the Fn injection. Fn is not killed by SNAP-generated NO in vitro. An increase in the total cell number was accompanied by an increase of the neutrophil numbers in the LB group. Intracellular O2(-) generation (including ONOO(-)) was visualized using dihydrorhodamine (DHR)-123. The peak of O2(-) generation by PEC was shown to be at 3 hr in all 3 groups. The number of O2(-) positive cells in the LB group at 3 hr was remarkably high, and most of them were likely to be neutrophils. The Fn reduction would be performed cooperatively via oxygen dependent and oxygen independent mechanisms. Thus reactive oxygen species (ROS) included in the oxygen dependent mechanism appear to be important for Fn reduction. However the significant amounts of NO derived from the iNOS synthesized in the LB group between 12 hr and 24 hr after injection of LFn were not involved in the Fn reduction.     

Pressure increases oxygen affinity of whole blood and erythrocyte suspensions

Effect of hydrostatic pressure (HP) on whole blood (WB) or erythrocyte suspension hemoglobin (Hb) O2 affinity has been studied using newly developed techniques. O2 partial pressure at which hemoglobin is half-saturated with O2 (P50) measurements were made at 5 HP (1, 26, 51, 76, and 126 ATA) on thin films of human WB or erythrocytes at 37 degrees C. CO2 partial pressure of WB was either 28 or 57 Torr (film pH 7.51 or 7.31). HP increased affinity of erythrocytes and WB. For erythrocytes in tris(hydroxymethyl)aminomethane buffer, the ratio (r) of P50 (1 ATA)/P50 (51 ATA) was 1.089 (P less than 0.01) at pH 7.0. WB P50 decreased with HP at a rate of -3.3 X 10(-2) Torr X atm-1; change in P50 at higher HP vs. 1 ATA was highly significant (P less than 0.01). No effect of HP was seen on the CO2 Bohr coefficient. Inert gas choice, N2 vs. helium (He), had no effect. Measurement of decrease of P50 with HP at 76 ATA in hemolyzed WB gave an r of 1.15, as great or greater than that found in WB, indicates that Donnan equilibrium alteration is not involved. No effect of HP was found in WB on the ratio of P50 of erythrocytes with normal (5 mmol/l erythrocytes) 2,3-diphosphoglycerate (DPG) to P50 of erythrocytes with less than 5% of normal DPG; i.e., no effect of pressure was seen on the independent influence of DPG on P50. WB measurements of Hb O2 uptake under simulated physiological conditions are characterized by a net decrease in partial molal volume on oxygenation of 30-35 ml/mol Hb4.