Aerobic Biotransformation of N-Nitrosodimethylamine and N-Nitrodimethylamine by Benzene-, Butane-, Methane-, Propane-, and Toluene-Fed Cultures

N-Nitrosodimethylamine (NDMA) is an emerging contaminant of concern. N-nitrodimethylamine (DMNA) is a structural analog to NDMA. NDMA and DMNA have been found in drinking water, groundwater, and other media and are of concern due their toxicity. The authors evaluated biotransformation of NDMA and DMNA by cultures enriched from contaminated groundwater growing on benzene, butane, methane, propane, or toluene. Maximum specific growth rates of enriched cultures on butane (μ_max = 1.1 h^?1) and propane (μ_max = 0.65 h^?1) were 1 to 2 orders of magnitude higher than those presented in the literature. Growth rates of mixed cultures grown on benzene (μ_max = 1.3 h^?1), methane (μ_max = 0.09 h^?1), and toluene (μ_max = 0.99 h^?1) in these studies were similar to those presented in the literature. NDMA biotransformation rates for methane oxidizers (υ_max = 1.4 ng min^?1 mg^?1) and toluene oxidizers (υ_max = 2.3 ng min^?1 mg^?1) were comparable to those presented in the literature, whereas the biotransformation rate for propane oxidizers (υ_max = 0.37 ng min^?1 mg^?1) was lower. NDMA biotransformation rates for benzene oxidizers (υ_max = 1.02 ng min^?1 mg^?1) and butane oxidizers (υ_max = 1.2 ng min^?1 mg^?1) were comparable to those reported for other primary substrates. These studies showed that DMNA biotransformation rates for benzene (υ_max = 0.79 ng min^?1 mg^?1), butane (υ_max = 1.0 ng min^?1 mg^?1), methane (υ_max = 2.1 ng min^?1 mg^?1), propane (υ_max = 1.46 ng min^?1 mg^?1), and toluene (υ_max = 0.52 ng min^?1 mg^?1) oxidizers were all comparable. These studies highlight potential bioremediation methods for NDMA and DMNA in contaminated groundwater.     

Biotic and abiotic immobilization of ammonium, nitrite, and nitrate in soils developed under different tree species in the Catskill Mountains, New York, USA

Nitrogen retention in soil organic matter (SOM) is a key process influencing the accumulation and loss of N in forest ecosystems, but the rates and mechanisms of inorganic N retention in soils are not well understood. The primary objectives of this study were to compare ammonium (NH₄⁺), nitrite (NO₂^?), and nitrate (NO₃^?) immobilization among soils developed under different tree species in the Catskill Mountains of New York State, and to determine the relative roles of biotic or abiotic processes in soil N retention. A laboratory experiment was performed, where ¹⁵N was added as NH₄⁺, NO₂^?, or NO₃^? to live and mercury‐treated O horizon soils from three tree species (American beech, northern red oak, sugar maple), and ¹⁵N recoveries were determined in the SOM pool. Mercuric chloride was used to treat soils as this chemical inhibits microbial metabolism without significantly altering the chemistry of SOM. The recovery of ¹⁵N in SOM was almost always greater for NH₄⁺ (mean 20%) and NO₂^? (47%) than for NO₃^? (10%). Ammonium immobilization occurred primarily by biotic processes, with mean recoveries in live soils increasing from 9% at 15 min to 53% after 28 days of incubation. The incorporation of NO₂^? into SOM occurred rapidly (<15 min) via abiotic processes. Abiotic immobilization of NO₂^? (mean recovery 58%) was significantly greater than abiotic immobilization of NH₄⁺ (7%) or NO₃^? (7%). The incorporation of NO₂^? into SOM did not vary significantly among tree species, so this mechanism likely does not contribute to differences in soil NO₃^? dynamics among species. As over 30% of the ¹⁵NO₂^? label was recovered in SOM within 15 min in live soils, and the products of NO₂^? incorporation into SOM remained relatively stable throughout the 28‐day incubation, our results suggest that NO₂^? incorporation into SOM may be an important mechanism of N retention in forest soils. The importance of NO₂^? immobilization for N retention in field soils, however, will depend on the competition between incorporation into SOM and nitrification for transiently available NO₂^?. Further research is required to determine the importance of this process in field environments.     

Ammonium, nitrate, and proton fluxes along the maize root

Ion-selective microelectrodes were used to measure NH₄⁺, NO₃^– and H⁺ fluxes along the primary root of maize seedlings. Plants were exposed to nutrient solutions containing NH₄⁺, NO₃^– or both ions. Nitrogen fluxes along the root varied substantially among the different treatments. Net NH₄⁺ and NO₃^– uptake and H⁺ extrusion were low at the very apex of the root and generally increased in the more basal regions. In the absence of nitrogen or in the presence of NO₃^– alone, net H⁺ uptake (and root surface alkalinization) occurred at the root tip (0–1 mm), whereas net H⁺ extrusion occurred in all other regions. In the presence of NH₄⁺ alone, a dramatic increase in net H⁺ extrusion was detected in all regions except for the region 6–11 mm from the apex. In contrast, when NO₃^– alone was supplied, net H⁺ extrusion was depressed at all locations except for the tip (0–1 mm). When both NH₄⁺ and NO₃^– were supplied, NO₃^– uptake was suppressed at all locations while net H⁺ extrusion was increased relative to NO₃^– alone. The capacities to absorb NH₄⁺ and NO₃^– at the tip were similar, as indicated by flux rates when NH₄⁺ or NO₃^– were supplied as sole sources, but when supplied together, net NO₃^– uptake was half that of net NH₄⁺ uptake, indicating that NH₄⁺ may satisfy the nitrogen requirements of the poorly vascularized apical tissue in the most energy-efficient way. The high spatial resolution of the measurements enabled us to establish that acidification in the root expansion zone is maintained regardless of nitrogen source.     

Distribution of nitrogen-15 tracers applied to the canopy of a mature spruce-hemlock stand,Howland, Maine,USA

In N-limited ecosystems, fertilization by N deposition may enhance plant growth and thus impact C sequestration. In many N deposition–C sequestration experiments, N is added directly to the soil, bypassing canopy processes and potentially favoring N immobilization by the soil. To understand the impact of enhanced N deposition on a low fertility unmanaged forest and better emulate natural N deposition processes, we added 18 kg N ha⁻¹ year⁻¹ as dissolved NH₄NO₃ directly to the canopy of 21 ha of spruce-hemlock forest. In two 0.3-ha subplots, the added N was isotopically labeled as ¹⁵NH₄ ⁺ or ¹⁵NO₃ ⁻ (1% final enrichment). Among ecosystem pools, we recovered 38 and 67% of the ¹⁵N added as ¹⁵NH₄ ⁺ and ¹⁵NO₃ ⁻, respectively. Of ¹⁵N recoverable in plant biomass, only 3–6% was recovered in live foliage and bole wood. Tree twigs, branches, and bark constituted the most important plant sinks for both NO₃ ⁻ and NH₄ ⁺, together accounting for 25–50% of ¹⁵N recovery for these ions, respectively. Forest floor and soil ¹⁵N retention was small compared to previous studies; the litter layer and well-humified O horizon were important sinks for NH₄ ⁺ (9%) and NO₃ ⁻ (7%). Retention by canopy elements (surfaces of branches and boles) provided a substantial sink for N that may have been through physico-chemical processes rather than by N assimilation as indicated by poor recoveries in wood tissues. Canopy retention of precipitation-borne N added in this particular manner may thus not become plant-available N for several years. Despite a large canopy N retention potential in this forest, C sequestration into new wood growth as a result of the N addition was only ~16 g C m⁻² year⁻¹ or about 10% above the current net annual C sequestration for this site.     

Induction of nitrate reductase, nitrite reductase, and glutamine synthetase isoforms in sunflower cotyledons as affected by nitrate, light, and plastid integrity

Summary We investigated the inducibility of nitrate reductase (NR; EC 1.6.6.1), nitrite reductase (NiR; EC 1.7.7.1), and glutamine synthetase (GS; EC 6.3.1.2) isoforms in cotyledons of 7-day-old seedlings of sunflower (Helianthus annuus L.) in relation to light, nitrogen source (NO ₃ ^– , NO ₂ ^– or NH ₄ ⁺ ), and the involvement of plastids. Nitrate was absolutely (and specifically) required for NR induction, and stimulated more effectively than NO ₂ ^– or NH ₄ ⁺ the synthesis of NiR and chloroplastic GS (GS₂) over the constitutive levels present in N-free-grown seedlings. In vivo inhibition of NR activity by tungsten application to seedlings and measurements of tissue NO ₃ ^– concentration indicate that NO ₃ ^– -dependent enzyme induction is elicited by NO ₃ ^– per se and not by a product of its assimilatory reduction, e.g., NO ₂ ^– or NH ₄ ⁺ . In the presence of NO ₃ ^– , light remarkably enhanced the appearance of NR, NiR, and GS₂, while the activity of the cytosolic GS isoform (GS₁) was adversely affected. Cycloheximide suppressed much more efficiently than chloramphenicol the light- and NO ₃ ^– -dependent increase of GS₂ activity, indicating that sunflower chloroplastic GS is synthesized on cytoplasmic 80S ribosomes. When the plastids were damaged by photooxidation in cotyledons made carotenoid-free by application of norflurazon, the positive action of light and NO ₃ ^– on the appearance of NR, NiR, and GS₂ isoform was greatly abolished. Therefore, it is suggested that intact chloroplasts are required for the inductive effect of light and NO ₃ ^– and/or for the accumulation of newly formed enzymes in the organelle.Abbreviations CAP chloramphenicol - CHX cycloheximide - GS glutamine synthetase - GS₁ cytosolic GS - GS₂ plastidic (chloroplastic) GS - NF norflurazon - NiR nitrite reductase - NR nitrate reductase     

Chromosomal assignment of a large tRNA gene cluster (tRNALeu,tRNAGln, tRNALys,tRNAArg, tRNAGly) to 17p13.1

Summary A cluster of tRNA genes (tRNA _UAG ^Leu , tRNA _CUG ^Gln , tRNA _UUU ^Lys , tRNA _UCU ^Arg ) and an adjacent tRNA _GCC ^Gly have been assigned to human chromosome 17p12–p13.1 by in situ hybridization using a 4.2 kb human DNA fragment for tRNA^Leu, tRNA^Gln, tRNA^Lys, tRNA^Arg, and, for tRNA^Gly, 1.3 kb and 0.58 kb human DNA fragments containing these genes as probes. This localization was confirmed and refined to 17p13.100–p13.105 using a somatic cell hybrid mapping panel. Preliminary experiments with the biotiny lated tRNA Leu, Gln, Lys, Arg probe and metaphase spreads from other great apes suggest the presence of a hybridization site on the long arm of gorilla (Gorilla gorilla) chromosome 19 and the short arm of orangutan (Pongo pygmaeus) chromosome 19 providing further support for homology between HSA17, GGO19 and PPY19.     

Selective inhibition of L-glutamate and gammaaminobutyrate transport in nerve ending particles by aluminium,manganese, and cadmium chloride

AlCl₃, MnCl₂, and CdCl₂ inhibited the rates of accumulation of ¹⁴C] L-glutamate and ³H] gammaaminobutyrate (GABA) in purified rat forebrain nerve-ending particles in a dose-dependent fashion. The concentrations that would give 50% inhibition (IC₅₀) of GABA transport were 316 μM, 7.4 mM, and 1.4 mM, respectively. Ca²⁺ (1 mM) enhanced the inhibitory effect of Al³⁺ (IC₅₀ decreased to 149 μM) but antagonized that of Mn²⁺ (IC₅₀ = 10 mM) and Cd²⁺ (IC₅₀ = 2.1 mM). For glutamate transport 1 mM Ca²⁺ changed the IC₅₀ values from 299 to 224 μm for Al³⁺, 7.1 to 10 mM for Mn²⁺, and 2 to 3 mM for Cd²⁺. In contrast, the rates of accumulation of ¹⁴C] 2-deoxy-glucose and ³H] L-phenylalanine were mostly unaffected by these metal ions. The results indicate that Al³⁺, Mn²⁺, and Cd²⁺ exerted selective and differential effects on the transport systems of neurotransmitter substances in the synaptosomal membrane.     

Coordinated 2-halo-l,3,2-dioxaphosphorinane ligands. I. syntheses and 13C, 17O, 31P and 95Mo NMR and IR spectroscopic characterization of some molybdenum pentacarbonyl complexes of 2-substituted-5, 5-dimethyl-1,3, 2-dioxaphosphorinanes

A study of the reactions of Mo(CO)₅(P(OCH₂- CMe₂CH₂0)X) (X = C1, Br) with a variety of nucleophiles of the type HER (E = NH, O, S; R = H, alkyl, aryl) is reported. The mechanism of these reactions is shown to be S_N2, and the significantly slower rates of reactions of n-propylamine with the above complexes relative to the rate of reaction of n-propylamine with Mo(CO)₅(Ph₂PC1) is discussed.The ¹³C, ¹⁷O, ³¹P and ⁹⁵Mo NMR data and infrared data for these complexes are presented. Good correlations between chemical shifts of the cis and trans CO¹³C and trans CO¹⁷0 NMR resonances, CO infrared stretching force constants and the magnitudes of ¹J_Mop and ²J_PC (trans CO) are observed and the reasons for these correlations are discussed.The correlations between the chemical shifts of NMR-active nuclei in the Mo(CO)₅(P(OCH₂CMe₂- CH₂O)ER) complexes with the chemical shifts of similar nuclei in the Mo(CO)₅(Ph₂PER) complexes fange from excellent to very poor. This indicates that the effects of-the P-substituents on the chemical shifts of the NMR-active nuclei in these complexes are not additive.     

Monovalent Cation Permeation through the Connexin40 Gap Junction Channel : Cs,Rb, K,Na, Li,TEA, TMA,TBA, and Effects of Anions Br,Cl, F,Acetate, Aspartate,Glutamate, and NO3

The unitary conductances and permeability sequences of the rat connexin40 (rCx40) gap junction channels to seven monovalent cations and anions were studied in rCx40-transfected neuroblastoma 2A (N2A) cell pairs using the dual whole cell recording technique. Chloride salt cation substitutions (115 mM principal salt) resulted in the following junctional maximal single channel current-voltage relationship slope conductances (γ_j in pS): CsCl (153), RbCl (148), KCl (142), NaCl (115), LiCl (86), TMACl (71), TEACl (63). Reversible block of the rCx40 channel was observed with TBA. Potassium anion salt γ_j are: Kglutamate (160), Kacetate (160), Kaspartate (158), KNO₃ (157), KF (148), KCl (142), and KBr (132). Ion selectivity was verified by measuring reversal potentials for current in rCx40 gap junction channels with asymmetric salt solutions in the two electrodes and using the Goldman-Hodgkin-Katz equation to calculate relative permeabilities. The permeabilities relative to Li⁺ are: Cs⁺ (1.38), Rb⁺ (1.32), K⁺ (1.31), Na⁺ (1.16), TMA⁺ (0.53), TEA⁺ (0.45), TBA⁺ (0.03), Cl⁻ (0.19), glutamate⁻ (0.04), and NO₃− (0.14), assuming that the monovalent anions permeate the channel by forming ion pairs with permeant monovalent cations within the pore thereby causing proportionate decreases in the channel conductance. This hypothesis can account for why the predicted increasing conductances with increasing ion mobilities in an essentially aqueous channel were not observed for anions in the rCx40 channel. The rCx40 effective channel radius is estimated to be 6.6 Å from a theoretical fit of the relationship of relative permeability and cation radius.     

Iron and nickel complexes with heterocyclic ligands: Stability,synthesis, spectral characterization,antimicrobial activity,acute and subacute toxicity

The synthesis and characterization by elemental analysis, emission atomic spectroscopy, TG measurements, magnetic measurements, FTIR, ¹H NMR, UV–visible spectra and conductivity of a series of iron (II) and nickel (II) complexes with two heterocyclic ligands (L¹(SMX): sulfamethoxazole and L²(MIZ): metronidazole) used in pharmaceutical field and with a new ligand derived benzoxazole (L³(MPBO): 2-(5-methylpyridine-2-yl)benzoxazole), were reported. The formulae obtained for the complexes are: [M(L¹)₂ Cl₂]·nH₂O, [M(L²)₂Cl₂(H₂O)₂]·H₂O and [M(L³)₂(OH)₂]·nH₂O. Stability constants of these complexes have been determined by potentiometric methods in water–ethanol (90:10, v/v) mixture at a 0.2 mol L^?1 ionic strength (NaCl) and at 25.0 ± 0.1 °C. Sirko program was used to determine the protonation constants as well as the binding constants of three species [ML₂H₂]²⁺, [ML₂] and [ML]²⁺. The antimicrobial activity of the ligands and complexes was evaluated in vitro against different human bacteria and fungi using agar diffusion method.Iron sulfamethoxazole complex showed a remarkable inhibition of bacteria growth especially on Staphylococcus aureus and P. aeruginosa. The iron metronidazole complex is active against yeasts especially on Candida tropicalis strain. Nickel complexes presented different antibacterial and antifungal behavior's against bacteria and fungal.The acute toxicity study revealed that the iron complexes are not toxic at 2000 mg/kg dose orally administrated.LD₅₀ for nickel complexes was determined using graphical method.No significant differences in the body weights between the control and the treated groups of both rat sexes in subacute toxicity study using for iron complexes. Hematological and clinical blood chemistry analysis revealed no toxicity effects of the iron complexes. Pathologically, neither gross abnormalities nor histopathological changes were observed for these complexes.     

COMPARISONS OF NITRATE UPTAKE, STORAGE, AND REDUCTION IN MARINE DIATOMS AND FLAGELLATES

Diatoms, but not flagellates, have been shown to increase rates of nitrogen release after a shift from a low growth irradiance to a much higher experimental irradiance. We compared NO₃ ^? uptake kinetics, internal inorganic nitrogen storage, and the temperature dependence of the NO₃ ^? reduction enzymes, nitrate (NR) and nitrite reductase (NiR), in nitrogen‐replete cultures of 3 diatoms (Chaetoceros sp., Skeletonema costatum, Thalassiosira weissflogii) and 3 flagellates (Dunaliella tertiolecta, Pavlova lutheri, Prorocentrum minimum) to provide insight into the differences in nitrogen release patterns observed between these species. At NO₃ ^? concentrations <40 μmol‐N·L ^{? 1}, all the diatom species and the dinoflagellate P. minimum exhibited saturating kinetics, whereas the other flagellates, D. tertiolecta and P. lutheri, did not saturate, leading to very high estimated K _s values. Above ～60 μmol‐N·L ^{? 1}, NO₃ ^? uptake rates of all species tested continued to increase in a linear fashion. Rates of NO₃ ^? uptake at 40 μmol‐N·L ^{? 1}, normalized to cellular nitrogen, carbon, cell number, and surface area, were generally greater for diatoms than flagellates. Diatoms stored significant amounts of NO₃ ^? internally, whereas the flagellate species stored significant amounts of NH₄ ⁺ . Half‐saturation concentrations for NR and NiR were similar between all species, but diatoms had significantly lower temperature optima for NR and NiR than did the flagellates tested in most cases. Relative to calculated biosynthetic demands, diatoms were found to have greater NO₃ ^? uptake and NO₃ ^? reduction rates than flagellates. This enhanced capacity for NO₃ ^? uptake and reduction along with the lower optimum temperature for enzyme activity could explain differences in nitrogen release patterns between diatoms and flagellates after an increase in irradiance.     

Trace metals in sea water. : C. S. Wong,Edward Boyle,Kenneth W. Bruland,J. D. Burton and Edward D. Goldberg. Nato Conference Series,Series IV: Marine Sciences,Volume 9, Plenum Press,New York and London,pp. xiv + 920, ISBN 0-306-41165-2, U.S. $ 115.00.

A comprehensive mechanism is proposed for the photolysis of transition metal complexes in equilibrium solutions. This involves the photo-oxidation, a possibility of energy transfer and several secondary thermal reactions, e.g. forward and back reactions with photochemically-formed H· radicals. The scheme includes the individual quantum yield (IQY) of each species. The photo-oxidations of FeSO₄, FeClO₄, FeCl₂ in aqueous acidic solutions were studied by continuous irradiation. The IQY of Fe_aq²⁺ (0.2), FeSo₄ (0.3), FeHSO₄⁺ (0.67), FeClO₄⁺ (0.06–0.2), FeCl⁺ (0.8), FeCl₂ (0.3) were determined. The IQY was found to be dependent on H⁺ concentration, due to competition with geminal recombination within the solvent cage. This dependence, and the efficiency of energy transfer between excited iron(III) species and iron(II) in ground state, are discussed.     

Luminescence properties of neodymium,samarium, and europium niobate and tantalate thin films

Thin films of lanthanide orthoniobate LnNbO₄ (LnNO) and orthotantalate LnTaO₄ (LnTO), (Ln = Nd, Sm, Eu) were fabricated using the sol–gel method with subsequent spin-coating on the PbZrO₃/Al₂O₃ substrate and annealing at 1000°C. X-ray diffraction patterns showed monoclinic M-LnNbO₄ or M´-LnTaO₄, which coexists with the orthorhombic or tetragonal phase. X-ray photoelectron spectroscopy demonstrated the presence of Nd³⁺, Sm³⁺/Sm²⁺ and Eu³⁺/Eu²⁺ ions. The luminescence properties of polymorphic films were investigated. Excitation spectra of PbZrO₃ interlayer represented broad bands at 410 and 550 nm that were assigned to charge transfer bands (CTB). In all films, the CTB broad band at ~275 nm related to charge transfer transition of Ln³⁺→O²⁻ and NbO₄³⁻ or TaO₄³⁻ groups. In excitation spectra, ⁴I_9/2→⁴G_5/2 (Nd³⁺), ⁶H_5/2→⁶P_3/2 (Sm³⁺) and ⁷F₀→⁵L₆ (Eu³⁺) transitions (at 585, 402 and 395 nm), respectively were found to be more intense than any other Ln³⁺ transition. The emission spectra showed narrow and intense bands at 1065, 600, and 614 nm that were ascribed to Nd³⁺, Sm³⁺, and Eu³⁺ 4f–f intraconfigurational transitions ⁴F_3/2→⁴I_11/2, ⁴G_5/2→⁶H_7/2, and ⁵D₀→⁷F₂, respectively. The excellent luminescence properties of films make them new potential groups for visible and/or near-infrared applications such as sensors and imaging equipment.     

Ion complexation in nonactin,monactin, and dinactin: A Raman spectroscopic study

The ability of the macrotetrolide nactins to complex selectivity with a wide variety of cations makes these ionophorous antibiotics important model systems for the study of biologic ionic transport. We report a Raman spectroscopic investigation of the Na⁺, K⁺, Rb⁺, Cs⁺, Tl⁺, NH₄⁺, NH₃OH⁺, C(NH₂)₃⁺, and Ba⁺⁺ complexes of nonactin, monactin, and dinactin in 4:1 (v/v) CH₃OH/CHCl₃ and in the solid state. The nactins display characteristic spectral changes upon complexation, some of which are specific for a given cation. In the K⁺, Rb⁺, Cs⁺, NH₃OH⁺, and C(NH₂)₃⁺ complexes, which are apparently isosteric, the ester carbonyl stretch frequency is found to be linearly proportional to the cation–carbonyl electrostatic interaction energy, as calculated from a simplified model. Deviations for the Na⁺, NH₄⁺, Tl⁺, and Ba⁺⁺ complexes are interpreted as arising from additional nonelectrostatic interactions. Additional information is obtained from other spectral regions and from measurements of depolarization ratios. Spectra of the nactin complexes differ from each other more in the solid state than in solution, reflecting the effects of crystalline contact forces.     

CHARACTERIZATION OF NITROGEN UPTAKE BY NATURAL POPULATIONS OF AUREOCOCCUS ANOPHAGEFFERENS (CHRYSOPHYCEAE) AS A FUNCTION OF INCUBATION DURATION,SUBSTRATE CONCENTRATION,LIGHT, AND TEMPERATURE1

Nitrogen uptake studies were conducted during an aestival “brown tide” bloom in Shinnecock Bay, Long Island, New York. The same station was sampled in late July and mid-August 1995 when Aureococcus anophagefferens composed >90% and 30–40% of the total cell density, respectively. Experiments were designed to examine the effect of incubation duration on the uptake kinetics, and the effect of light and temperature dependencies of NH₄⁺, urea, and NO₃^? uptake. Maximum specific uptake rates (V'_max) decreased in the order NH₄⁺, urea, NO₃^? and were nonlinear with time for NH₄⁺ and urea, both of which exhibited an exponential decline between 1 and 10 min and then did nut significantly change for 60 min. Nitrogen uptake kinetic experiments exhibited a typical hyperbolic response for urea and NO₃^?. Half-saturation constants. (K_s) were calculated to he 0.03 and 0.12 μmol · L^?1 for urea and NO₃^?; respectively, but could not be calculated for NH₄⁺ under these experimental conditions. Nutrient uptake rate versus, irradiance (NI) experiments showed that maximum uptake rates occurred at ≤% of incident irradiance on both sampling dates and that values of V′_max-cell (NH₄⁺) were on average 30% greater than V′_max-cell (urea). A7°–9°C temperature decrease in incubation temperature between the two NI experiments in August resulted in a 30% decrease in V′_max-cell(NH₄⁺), no change in V′_max-cell(urea), and a 3–4-fold decrease in calculated K_lt values for both NH₄⁺ and urea. The results from these experiments demonstrate that A. anophagefferens has a higher affinity for NH₄⁺ and urea than for NO₃^? and that this particular species is adapted to use these substrates at low irradiances and concentrations. The data presented in this study are also consistent with the hypothesis that A. anophagefferens may be an oceanic clone that was displaced by an anomalous oceanographic event.     

Uptake and loss of nitrite from the blood of rainbow trout, Salmo gairdneri Richardson, and Atlantic salmon, Salmo salar L. in fresh water and in dilute sea water

The acute toxicity of nitrite (NO^?₂) to salmonids is strongly ameliorated by chloride (Cl^?) ions rendering it almost harmless in most fresh waters apart from those with low Cl^? content. In Cl^? poor fresh water external NO^?₂ is concentrated in the blood plasma until it is at approximately the same molar concentration as haemoglobin (about 8 mmol) and at this point most of the haemoglobin has been oxidized to methaemoglobin this being a contributory cause of death. Two theories are advanced to account for NO^?₂ concentration in the blood. The first supposes that gills are impermeable to NO^?₂ but allow its conjugate acid nitrous acid (HNO₂) to diffuse into the blood where it dissociates according to the blood pH value. Thus NO^?₂ will accumulate in the blood plasma if it has a higher pH value than the water. The second supposes that the Cl^? uptake mechanism in the freshwater gill has an affinity for NO^?₂ and accounts for the fact that NO^?₂ entry to the blood is suppressed when external Cl^? is present in significant amounts. The results also suggest that NO^?₂ and Cl^? behave similarly as diffusing ions. Thus NO^?₂ diffusion into the blood of seawater fish and from the blood of NO^?₂ loaded freshwater fish occurs at approximately the same rate as the corresponding Cl^? fluxes. Nitrite loss from seawater fish is thought to be mainly by diffusion although there is some evidence for the active Cl^? extrusion mechanism having a weak affinity for nitrite.     

Atmospheric deposition, mass balances, and processes regulating streamwater solute concentrations in mixed-conifer catchments of the Sierra Nevada, California

Solute concentrations in atmospheric deposition and stream water were measuredfrom 1984 through 1993 to determine the fate and mobility of solutes in twogauged mixed-conifer catchments (Tharp's and Log creeks) located in theSierra Nevada, California. The two catchments contain mature forest standsdominated by Abies concolor (white fir), Sequoiadendron giganteum (giantsequoia), Abies magnifica (red fir) and Pinus lambertiana (sugar pine).Ammonium, Cl^-, Ca²⁺ and NO^- ₃were highest in concentration of the solutes measured in wet deposition;bulk deposition was highest in SO^{2- 4}, NH⁺ ₄,Cl^- and H⁺. Net retention ofH⁺, NO₃ ^-, NH₄ ⁺,SO₄ ^2- and Cl^- occurred in both catchments.Discharge was dominated by spring snowmelt with the largest export yieldsfor acid neutralizing capacity (ANC), SiO₂, andCa²⁺. Export yields of H⁺,NO₃ ^-, NH₄ ⁺ and PO₄ ^3-were relatively small (0.5 kg ha^-1 y^-1).Discharge-concentration relationships for ANC, SiO₂,Na⁺, K⁺, Ca²⁺ andMg²⁺ were inverse and their concentrations in stream waterwere primarily influenced by discharge and annual differences in the relativecontributions of snowmelt and groundwater. The mobility of these solutes iscontrolled by the rates of mineral weathering and ion exchange. The positiverelationship of SO₄ ^2- concentration with increasingdischarge suggests that atmospherically deposited SO₄ ^2-is temporarily stored and that its release is controlled by the extent of soilwater flushing.     

Seasonal and spatial patterns of S,Ca, and N dynamics of a Northern Hardwood forest ecosystem

Seasonal dynamics of S, Ca and N were examined at the Huntington Forest, a northern hardwood ecosystem in the central Adirondacks of New York for a period of 34 months (1985–1988). Solute concentrations and fluxes in bulk precipitation, throughfall (TF) and leachates from the forest floor, E horizon and B horizon were quantified. Both above and below-ground elemental fluxes mediated by vegetation (e.g. uptake, litter inputs, and fine roots production) were also determined. The roles of abiotic and biotic processes were ascertained based on both changes in solute concentrations through the strata of the ecosystem as well as differences between dormant and growing seasons. Concentrations of SO₄ ²⁻, NO₃ ⁻, NH₄ ⁺ and Ca²⁺ were greater in TF than precipitation. Forest floor leachates had greater concentrations of SO₄ ²⁻, NO₃ ⁻ + NH₄ ⁺ and Ca²⁺ (9, 6 and 77 μeq L⁻¹, respectively) than TF. There were differences in concentrations of ions in leachates from the forest floor between the dormant and growing seasons presumably due to vegetation uptake and microbial immobilization. Concentrations and fluxes of NO₃ ⁻ and NH; were greatest in early spring followed by a rapid decline which coincided with a demand for N by vegetation in late spring. Vegetation uptake (44.7 kg N ha⁻¹ yr⁻¹ ) could account for the low leaching rates of N0₃ ⁻. Within the mineral soil, changes with soil depth and the absence of seasonal patterns suggest that cation exchange (Ca⁺) or anion sorption (SO₄ ²⁻) are primarily responsible for regulating solute concentrations. The increase in SO₄ ²⁻ concentration after leachates passed through the mineral soil may be attributed to desorption of sulfate that was adsorbed during an earlier period when SO₄ ²⁻ concentrations would have been greater due to elevated S inputs.     

Nutrient cycling in shallow,oligotrophic Lake Kvie,Denmark

The importance of isoetids for the exchange of dissolved inorganic nitrogen (DIN) between sediment and water was studied in shallow Lake Kvie, Denmark. Vegetated sediments from the littoral zone (55% of lake area) were compared to unvegetated sediments from the littoral and profundal zone. Clear effects of the isoetids were found on DIN in the porewater. At the vegetated station, NH₄ ⁺ showed the highest concentrations just below the surface (< 40 µM) whereas NO₃ ^- was dominating below 5 cm depth with concentrations up to 100 µM during the spring. The unvegetated littoral sediment showed a distinct change between winter where NH₄ ⁺ dominated and summer where NO₃ ^- was most abundant. NH₄ ⁺ dominated in the profundal sediment and showed increasing concentration with depth. The E_h was high (> 400 mV) in the vegetated sediment, indicating isoetid release of O₂ in the rhizosphere. A low DIN uptake was observed at the vegetated station while, based on porewater data, a diffusive release from the sediment was expected. This difference was due to plant assimilation. In general a release of NH₄ ⁺ and an uptake of NO₃ ^- was seen in all sediments. The denitrification rate calculated from the mass balance for the entire lake was 0.4 mmol m - 2 d^-1 and accounted for removal of 77% of the annual N-input to Lake Kvie.     

Highly flexible O,O′,N ligands and their Fe, Ni, Cu and Zn complexes

Three new chiral ligands bearing an O,O′,N donor set (O_methoxyO_hydroxyN_pyridine) were synthesised and coordinated to Fe^III, Fe^II, Ni^II, Cu^II and Zn^II to yield complexes with the general formula [M(OON)Cl_x]_y. While the pyridine N and the hydroxy O atoms coordinate strongly to all applied metal ions, the methoxy donor seems not to be involved in coordination, although some evidence for a weak interaction between O_Me and the Zn^II were found in NMR spectra. In the bidentate O′,N coordination mode the new ligands exhibit several coordination geometries as analysed in the solid compounds by XRD, EXAFS and EPR and in solution by UV-Vis absorption, cyclic voltammetry, EXAFS, EPR or NMR spectroscopy.