Photophysical and electrochemical properties of a dysprosium‐zinc tetra(4‐sulfonatophenyl)porphyrin complex

A dysprosium‐zinc porphyrin, [DyZn(TPPS)H₃O]_n (1) (TPPS = tetra(4‐sulfonatophenyl)porphyrin), was prepared through solvothermal reactions and structurally characterized by single‐crystal X‐ray diffraction analyses. Complex 1 features a three‐dimensional (3‐D) porous open framework that is thermally stable up to 400 °C. Complex 1 displays a void space of 215 ų, occupying 9.2% of the unit cell volume. The fluorescence spectra reveal that it shows an emission band in the red region. The fluorescence lifetime is 39 µsec and the quantum yield is 1.7%. The cyclic voltammetry (CV) measurement revealed one quasi‐reversible wave with E_1/2 = 0.30 V. Copyright © 2015 John Wiley & Sons, Ltd.     

Direct and Indirect Effects of Mutations at the Outer Mouth of the Cystic Fibrosis Transmembrane Conductance Regulator Chloride Channel Pore

The cystic fibrosis transmembrane conductance regulator (CFTR) Cl⁻ channel pore is thought to contain multiple binding sites for permeant and impermeant anions. Here, we investigate the effects of mutation of different positively charged residues in the pore on current inhibition by impermeant Pt(NO₂)₄²⁻ and suramin anions. We show that mutations that remove positive charges (K95, R303) influence interactions with intracellular, but not extracellular, Pt(NO₂)₄²⁻ ions, consistent with these residues being situated within the pore inner vestibule. In contrast, mutation of R334, supposedly located in the outer vestibule of the pore, affects block by both extracellular and intracellular Pt(NO₂)₄²⁻. Inhibition by extracellular Pt(NO₂)₄²⁻ requires a positive charge at position 334, consistent with a direct electrostatic interaction resulting in either open channel block or surface charge screening. In contrast, inhibition by intracellular Pt(NO₂)₄²⁻ is weakened in all R334-mutant forms of the channel studied, inconsistent with a direct interaction. Furthermore, mutation of R334 had similar effects on block by intracellular suramin, a large organic molecule that is apparently unable to enter deeply into the channel pore. Mutation of R334 altered interactions between intracellular Pt(NO₂)₄²⁻ and extracellular Cl⁻ but not those between intracellular Pt(NO₂)₄²⁻ and extracellular Pt(NO₂)₄²⁻. We propose that while the positive charge of R334 interacts directly with extracellular anions, mutation of this residue also alters interactions with intracellular anions by an indirect mechanism, due to mutation-induced conformational changes in the protein that are propagated some distance from the site of the mutation in the outer mouth of the pore.     

An Anionic Porphyrin Binds <Emphasis Type="Italic">β</Emphasis>-Lactoglobulin A at a Superficial Site Rich in Lysine Residues

Binding of small ligands to globular proteins remains a major research topic in biophysics. We have studied the binding of several photoactive dyes to β-lactoglobulin (BLG), as a model to investigate the photoinduced effects of porphyrins on proteins. A combination of optical spectroscopies (fluorescence, circular dichroism) and molecular docking simulations were used to estimate the pH-dependence of the binding parameters and the docking location for meso-tetrakis(sulfonatophenyl)-porphyrin (TPPS). We have observed that the binding of TPPS is not modulated by the pH-mediated conformational transition of the protein (i.e., Tanford transition). Binding of TPPS appears to occur with some degree of negative cooperativity. Moreover, TPPS remains bound even upon partial denaturation of the protein. These results are consistent with a superficial binding site at a location removed from the aperture of the interior β-barrel. Binding occurs through electrostatic interactions between the negative SO₃ ⁻ groups of TPPS and positively charged Lys and Arg residues. This is the first study that explores the interaction of an anionic porphyrin with BLGA in a pH range that spans across the Tanford transition. Establishing the location of the binding site will enable us to explain the photoinduced conformational effects mediated by TPPS on BLG. Electronic supplementary material  The online version of this article (doi:) contains supplementary material, which is available to authorized users.     

Synthesis and Properties of a Clean and Sustainable Deicing Additive for Asphalt Mixture

A clean and sustainable deicing additive was prepared via the adsorption of acetate anions (Ac^-) by magnesium (Mg) and aluminum (Al) calcined layered double hydroxide (Mg/Al-CLDH). Fourier transform infrared spectroscopy spectrums proved that Ac^- had intercalated into LDH structure. X-ray diffraction patterns, scanning electron microscopy and transmission electron microscopy images showed that the intercalation spacing and platelet thickness of Mg and Al layered double hydroxide containing Ac^- anions (Mg/Al-Ac^- LDH) had been enlarged due to substitution of divalent CO₃ ^2- anions by a larger quantity of monovalent Ac^– anions. Differential scanning calorimetry tests testified that the insoluble Mg2/Al-Ac^- LDH evidently decreased the freeze point (FP) of water to -10.68°C. X-ray photoelectron spectroscopy analyses confirmed that the Ac- were strongly confined by the metal layers of LDHs. FP test of asphalt mixtures confirmed that Mg/Al-Ac^- LDHs reduced FP to -5.5°C. Immersion test results indicated that Mg/Al-Ac^- LDH had a good deicing durability and Ac^- did not released from asphalt mixture. Snow melting observation was conducted further testified that Mg/Al-Ac^- LDH melted snow or ice sustainably.     

Interactions between Impermeant Blocking Ions in the Cystic Fibrosis Transmembrane Conductance Regulator Chloride Channel Pore: Evidence for Anion-Induced Conformational Changes

It is well known that extracellular Cl⁻ ions can weaken the inhibitory effects of intracellular open channel blockers in the cystic fibrosis transmembrane conductance regulator (CFTR) Cl⁻ channel pore. This effect is frequently attributed to repulsive ion-ion interactions inside the pore. However, since Cl⁻ ions are permeant in CFTR, it is also possible that extracellular Cl⁻ ions are directly competing with intracellular blocking ions for a common binding site; thus, this does not provide direct evidence for multiple, independent anion binding sites in the pore. To test for the possible through-space nature of ion-ion interactions inside the CFTR pore, we investigated the interaction between impermeant anions applied to either end of the pore. We found that inclusion of low concentrations of impermeant Pt(NO₂)₄²⁻ ions in the extracellular solution weaken the blocking effects of three different intracellular blockers [Pt(NO₂)₄²⁻, glibenclamide and 5-nitro-2-(3-phenylpropylamino)benzoic acid] without affecting their apparent voltage dependence. However, the effects of extracellular Pt(NO₂)₄²⁻ ions are too strong to be accounted for by simple competitive models of ion binding inside the pore. In addition, extracellular Fe(CN)₆³⁻ ions, which do not appear to enter the pore, also weaken the blocking effects of intracellular Pt(NO₂)₄²⁻ ions. In contrast to previous models that invoked interactions between anions bound concurrently inside the pore, we propose that Pt(NO₂)₄²⁻ and Fe(CN)₆³⁻ binding to an extracellularly accessible site outside of the channel permeation pathway alters the structure of an intracellular anion binding site, leading to weakened binding of intracellular blocking ions.     

Structure analysis of hydrotalcite intercalated with pyrenetetrasulfonate; experiments and molecular modelling

The structure of pyrenetetrasulfonate intercalated with hydrotalcite, having the formula [Zn_0.68Al_0.32(OH)₂][(C₁₆H₆O₁₂S₄)_0.08 · x H₂O], was proposed based on molecular simulations combined with experimental data (X-ray powder diffraction, thermogravimetry). Calculations were done for samples kept at various relative humidities (0%, 84%, 98%). The appropriate models were selected from comparison of calculated and measured diffraction patterns. Modelling revealed the arrangement of pyrenetetrasulfonate anions, and the positions and the amount of water molecules in the interlayer space of the host structure. The results confirmed a large variability in the arrangement of the guest species. In the sample without water molecules (0% RH), pyrenetetrasulfonate anions formed a layer at the centre of the interlayer distance. For the sample kept at 84% RH, the anions formed two layers at the thirds of the interlayer. For the sample kept at 98% RH, the anions became tilted with respect to the layered double hydroxides (LDH) layers and are less organised. Water molecules were arranged in three distinct planes: one in the middle and two at the quarters of interlayer distance. The number of water molecules obtained by the modelling basically agrees with the water content as measured by thermogravimetry. Figure Pyrenetetrasulfonate was intercalated into hydrotalcite and equilibrated at various relative humidities. Structural analysis was performed using molecular simulations based on X-ray and thermogravimetric data     

Anion effects on the structural organization of spinach thylakoid membranes

Changes in the conformation of spinach thylakoid membranes were monitored in 5-doxyl stearic acid (SAL)-treated thylakoid membranes in the presence of various anions (Cl⁻, Br⁻, I⁻, NO₂ ⁻, SO₄ ²⁻, PO₄ ³⁻). The presence of anions made the thylakoid membrane more fluid. The extent of change in membrane fluidity differed with different anion and was reversible.     

Relationship between river water quality and land use in a small river basin running through the urbanizing area of Central Japan

In this study, the relationship between water quality (as represented by major inorganic ion concentrations) and land use characteristics is examined for a small river basin which runs through the urbanizing area of central Japan. Water samples were taken from 24 sites at base flow and analyzed, and the proportions of the various land uses associated with the respective drainage basins were calculated using a digital land-use map (scale: 1:25000). The electrical conductivity (EC) of the water ranged from 84.5 to 600 μS cm⁻¹. Ca²⁺ and Na⁺ were the major cations, accounting for 77% of all cations. Among the anions, HCO₃ ⁻ was dominant (56%), followed by Cl⁻ (24%), SO₄ ²⁻ (13%) and NO₃ ⁻ (7%). Applying principal component analysis to land use in the drainage basin yielded three principal components. The first principal component expressed the degree of occupation by residential areas, the second indicated the degree of urban developing area (i.e., fast-developing and industrial areas), and the third showed the degree of coverage with farmland and green space. The residential area showed significant positive correlations with K⁺, Mg²⁺, Ca²⁺, NO₃ ⁻, HCO₃ ⁻, EC and TMI (total major ions). Urban developing area showed significant positive correlations with Ca²⁺, Cl⁻, HCO₃ ⁻, EC and TMI as well as weak negative correlations with NO₃ ⁻ and SO₄ ²⁻. Industrial area showed weak positive correlations with Na⁺ and Cl⁻ and a moderate negative correlation with NO₃ ⁻. Farmland showed significant positive correlations with NO₃ ⁻ and SO₄ ²⁻; these ions are present due to fertilizers and the biological activity of plants. Forest area is inversely related to almost all ions, indicating the need for this form of land use in order to maintain river water quality.     

Superlattice Formation of Crystal Water in Layered Double Hydroxides for Long‐Term and Fast Operation of Aqueous Rechargeable Batteries

Aqueous rechargeable batteries (ARBs) are gaining increasing attention as alternatives to conventional nonaqueous lithium ion batteries. However, finding electrode materials with competitive electrochemical properties in various aspects is challenging. Moreover, the operation mechanism of some of high performance electrode materials is not fully understood. Here, an α‐phase layered double hydroxide (α‐LDH) working in alkaline electrolytes as an ARB cathode is reported. On charge, OH^? carrier ions intercalate into the interlayer space and react with protons detached from the host structure to yield crystal water. This crystal water is then arranged in a superlattice during charging to accommodate carrier ions and stabilize the structure. The solid solution mixing of cobalt and nickel also stabilizes the structure during the wide range of redox swing of Ni from 2+ to 4+. In pairing with Fe₃O₄/Fe(OH)₂ mixture, the α‐LDH exhibits 198.0 mA h g^?1 at 3 A g^?1, 68.3% capacity retention after 10 000 cycles, and 172.5 mA h g^?1 at 1 min charge, demonstrating the promise of hydrated compounds for ARB electrodes. The present study elucidates that the arrangement of crystal water within the host framework plays a critical role in determining the electrochemical performance of the corresponding hydrated active compound in aqueous media.     

Biological effects of anionic meso-tetrakis (para-sulfonatophenyl) porphyrins modulated by the metal center. Studies in rat liver mitochondria

In this paper, we present a study about the influence of the porphyrin metal center and meso ligands on the biological effects of meso-tetrakis porphyrins. Different from the cationic meso-tetrakis 4-N-methyl pyridinium (Mn(III)TMPyP), the anionic Mn(III) meso-tetrakis (para-sulfonatophenyl) porphyrin (Mn(III)TPPS4) exhibited no protector effect against Fe(citrate)-induced lipid oxidation. Mn(III)TPPS4 did not protect mitochondria against endogenous hydrogen peroxide and only delayed the swelling caused by tert-BuOOH and Ca²⁺. Fe(III)TPPS4 exacerbated the effect of the tert-BuOOH, and both porphyrins did not significantly affect Fe(II)citrate-induced swelling. Consistently, Fe(III)TPPS4 predominantly promotes the homolytic cleavage of peroxides and exhibits catalytic efficiency ten-fold higher than Mn(III)TPPS4. For Mn(III)TPPS4, the microenvironment of rat liver mitochondria favors the heterolytic cleavage of peroxides and increases the catalytic efficiency of the manganese porphyrin due to the availability of axial ligands for the metal center and reducing agents such as glutathione (GSH) and proteins necessary for Compound II (oxomanganese IV) recycling to the initial Mn(III) form. The use of thiol reducing agents for the recycling of Mn(III)TPPS4 leads to GSH depletion and protein oxidation and consequent damages in the organelle.     

Effects of N source on pH and nutrient exchange of extramatrical mycelium in a mycorrhizal Ri T-DNA transformed root system

 The influence of different N sources on medium pH variation and the effect of the external mycelium of arbuscular mycorrhizal fungi on nutrient dynamics were studied using a two-compartment, aseptic Petri plate system. VA mycorrhizal, transformed roots of carrot (Daucus carota L.) were cultured in the proximal compartment and external mycorrhizal mycelium in the distal compartment. The medium in the distal compartament contained N either as NO₃ ^– or as NH₄ ⁺. The pH and the anion and cation concentrations were measured every 15 days in filtrates prepared from the distal compartments. Thirteen weeks after colonization, there was a significant basification or a light acidification of the NO₃ ^– and NH₄ ⁺ medium, respectively. There was no change in NO₃ ^– concentration but a significant decrease in NH₄ ⁺ concentration. Treatments containing N as NO₃ ^– showed no variation in cations such asCa²⁺ and Mg²⁺ or anions such as PO₄ ^2–, and SO₄ ^2– but showed significant increases in the concentration of K⁺. Treatments containing N as NH₄ ⁺ showed no variation in cations or anions, except for increases in the concentrations of K⁺ and Cl^–. Accepted: 7 March 1996     

Riparian control on NO3 −, DOC, and dissolved Fe concentrations in mountainous streams, northern Japan

We evaluated (1) the longitudinal pattern of stream chemistry and (2) the effects of the riparian zone on this longitudinal pattern for nitrate (NO₃ ⁻), dissolved organic carbon (DOC), and total dissolved iron (Fe). We selected two small watersheds; the “southern watershed” had an extending riparian wetland and the “northern watershed” had a narrow riparian area. Stream NO₃ ⁻ concentrations decreased from the spring to outlet of both watersheds. In the southern watershed, stream DOC concentration decreased from the spring to midstream and then increased to the outlet. Stream Fe concentration in the southern watershed longitudinally increased. On the other hand, the northern watershed exhibited no longitudinal pattern for DOC and Fe concentrations. In both watersheds, while NO₃ ⁻ concentrations in the soil and ground water were lower than those in the stream waters, DOC and Fe concentrations exhibited the opposite patterns. The longitudinal decreases of NO₃ ⁻ concentrations in both streams and increase of stream Fe in the southern watershed mainly resulted from the inflow of the soil and ground water to the stream. The decrease in stream DOC from the spring to midstream in the southern watershed was due to the deep groundwater having low DOC, while the subsequent increase to the surrounding soil and ground water. Moreover, considerations of stream solute flow with soil and ground water chemistry suggested other mechanisms adding NO₃ ⁻ and removing/diluting DOC and Fe, especially for the northern watershed; coexistence of oxidizing and reducing conditions in the riparian zone might control the longitudinal concentration change in the stream water chemistry.     

The effect of solvated ions on the thermal denaturation of human serum albumin in water-dimethylsulfoxide solutions

The effects of solvated ions on the thermal denaturation of human serum albumin (HAS) in water-dimethylsulfoxide (DMSO) solutions were studied by the method of electron absorption spectroscopy. It was shown that depending on the DMSO concentration, electrolytes (LiCl, LiNO₃, LiClO₄, NaCl, and NaNO₃) contained in these solutions were characterized by different anion and cation solvation degrees: unlike cations, anions were only negligibly solvated, which affected HAS thermal denaturation. Electrostatic interactions between anions and positively charged amino acid residues supporting protein denaturation subsided in the line Cl⁻ > NO₃⁻ > ClO₄⁻.     

Effects of Anions on the Capacity and Affinity of Copper Adsorption in Two Variable Charge Soils

Effects of nitrate,(NO₃⁻) chloride (Cl⁻), sulfate (SO₄^2-, and acetate (Ac⁻) on Cu²⁺ adsorption and affinity of the adsorbed Cu²⁺ were evaluated in two Fe and Al enriched variable charge soils from Southern China. The maximum adsorption of Cu²⁺ (M, a parameter from the Langmuir isotherm model) in the presence of different anions decreased in the order Cl⁻ > Ac⁻ > NO₃⁻ > SO₄^2- for both soils. The clayey loamy soil (mixed siliceous thermic Typic Dystrochrept, TTD), developed on the Arenaceous rock, adsorbed less Cu²⁺ than the clayey soil (kaolinitic thermic Plinthudults, KTP), derived from the Quaternary red earths, regardless of anion type present in the medium. The affinity of adsorbed Cu²⁺ to both soils could be characterized by the Kd (distribution coefficient) values and successive extraction of the adsorbed Cu²⁺ with 1-mol NH₄Ac L⁻¹. The log₁₀Kd value was smaller for the TTD soil than for the KTP soil and decreased in the order of Cl⁻ > NO₃⁻ > SO₄^2- > Ac⁻ at low initial Cu²⁺ concentrations (≤40 mg Cu²⁺L⁻¹), whereas at 80 mg Cu²⁺L⁻¹, the log₁₀Kd value was similar for NO₃⁻, SO₄^2-, and Ac⁻, but was slightly higher for Cl⁻. Complete extraction of Cu²⁺ adsorbed in the presence of Ac⁻ was achieved. Influence of NO₃⁻ and SO₄^2- on the affinity of adsorbed Cu²⁺ was similar, but the effects of Cl⁻ depended on the initial Cu²⁺ concentrations. The extracted percentage of the adsorbed Cu²⁺ in the presence of NO₃⁻ or SO₄^2- increased with increasing Cu²⁺ adsorption saturation. The presence of Cl⁻, NO₃⁻, or SO₄^2- markedly decreased the equilibrium solution pH for both soils with increasing initial Cu²⁺ concentrations, and the delta pH values at the highest Cu²⁺ level were 0.5, 0.63, and 0.55 U for the TTD soil and 0.79, 0.84, and 0.93 U for the KTP soil, respectively for the three anions. The presence of Ac⁻ had a minimal influence on the equilibrium solution pH because of the buffering nature of the NaAc/HAc medium which buffered the released protons. The effects of anions on Cu²⁺ adsorption and affinity of the adsorbed Cu²⁺ were dependent on anion types and were apparently related to the altered surface properties caused by anion adsorption and/or the formation of anion– Cu²⁺ complexes.     

Cyanide Self-Addition,Controlled Adsorption,and Other Processes at Layered Double Hydroxides

Layered double hydroxides (LDH) are anion-exchangingmaterials of the type M(III)-M(II)_x(OH)_(2x+2)Y thatoccur abundantly in nature, and can concentrate, protect, andactivate simple organic anionic species of possible relevance tothe earliest organisms. We now wish to report progress in thefollowing areas:1) Internal vs. external uptake of anions. Ferrocyanidedoes not displace carbonate from synthetic hydrotalcite (Mg:AlLDH carbonate) but is nevertheless taken up on the outside of theparticles. In other cases, anion uptake is controlled byspecific hydrogen bonding requirements rather than by chargedensity alone, a feature that can be used to control whetheruptake will be both internal and external, or external only. These two findings taken together have important implications forspecific catalysis by LDH, since specific hydrogen bonding willaffect the individual and relative conformations of substrateanions, and anions occupying space in the interlayer will beunder tighter constraints than those adsorbed externally.2) Specific reactions catalyzed by LDH. We have found thatthe LDH Mg₂Al(OH)₆Cl catalyzes the self-addition ofcyanide, to give in a one-pot reaction at low concentrations anincreased yield of diaminomaleonitrile and in addition, at higher( 0.05M) concentrations, a purple-pink material that adheres tothe LDH. We are investigating whether this reaction also occurswith hydrotalcite itself, what is the minimum effectiveconcentration of cyanide, and what can be learned about theproducts and how they compare with those reported at high HCNconcentrations in the absence of catalyst.     

Effects of NO2? and NO3? on the Fe(III)EDTA reduction in a chemical absorption–biological reduction integrated NOx removal system

The biological reduction of Fe(III) ethylenediaminetetraacetic acid (EDTA) is a key step for NO removal in a chemical absorption–biological reduction integrated process. Since typical flue gas contain oxygen, NO₂ ⁻ and NO₃ ⁻ would be present in the absorption solution after NO absorption. In this paper, the interaction of NO₂ ⁻, NO₃ ⁻, and Fe(III)EDTA reduction was investigated. The experimental results indicate that the Fe(III)EDTA reduction rate decrease with the increase of NO₂ ⁻ or NO₃ ⁻ addition. In the presence of 10 mM NO₂ ⁻ or NO₃ ⁻, the average reduction rate of Fe(III)EDTA during the first 6-h reaction was 0.076 and 0.17 mM h⁻¹, respectively, compared with 1.07 mM h⁻¹ in the absence of NO₂ ⁻ and NO₃ ⁻. Fe(III)EDTA and either NO₂ ⁻ or NO₃ ⁻ reduction occurred simultaneously. Interestingly, the reduction rate of NO₂ ⁻ or NO₃ ⁻ was enhanced in presence of Fe(III)EDTA. The inhibition patterns observed during the effect of NO₂ ⁻ and NO₃ ⁻ on the Fe(III)EDTA reduction experiments suggest that Escherichia coli can utilize NO₂ ⁻, NO₃ ⁻, and Fe(III)EDTA as terminal electron acceptors.     

Sampling spatial and temporal variation in soil nitrogen availability

There are few studies in natural ecosystems on how spatial maps of soil attributes change within a growing season. In part, this is due to methodological difficulties associated with sampling the same spatial locations repeatedly over time. We describe the use of ion exchange membrane spikes, a relatively nondestructive way to measure how soil resources at a given point in space fluctuate over time. We used this method to examine spatial patterns of soil ammonium (NH⁺ ₄) and nitrate (NO⁻ ₃) availability in a mid-successional coastal dune for four periods of time during the growing season. For a single point in time, we also measured soil NH⁺ ₄ and NO⁻ ₃ concentrations from soil cores collected from the mid-successional dune and from an early and a late successional dune. Soil nitrogen concentrations were low and highly variable in dunes of all ages. Mean NH⁺ ₄ and NO⁻ ₃ concentrations increased with the age of the dune, whereas coefficients of variation for NH⁺ ₄ and NO⁻ ₃ concentrations decreased with the age of the dune. Soil NO⁻ ₃ concentration showed strong spatial structure, but soil NH⁺ ₄ concentration was not spatially structured. Plant-available NH⁺ ₄ and NO⁻ ₃ showed relatively little spatial structure: only NO⁻ ₃ availability in the second sampling period had significant patch structure. Spatial maps of NH⁺ ₄ and NO⁻ ₃ availability changed greatly over time, and there were few significant correlations among soil nitrogen availability at different points in time. NO⁻ ₃ availability in the second sampling period was highly correlated (r = 0.90) with the initial soil NO⁻ ₃ concentrations, providing some evidence that patches of plant-available NO⁻ ₃ may reappear at the same spatial locations at irregular points in time. Received: 20 February 1998 / Accepted: 23 November 1998     

Nitrate and nitrite inhibition of methanogenesis during denitrification in granular biofilms and digested domestic sludges

Anaerobic bioreactors that can support simultaneous microbial processes of denitrification and methanogenesis are of interest to nutrient nitrogen removal. However, an important concern is the potential toxicity of nitrate (NO₃ ⁻) and nitrite (NO₂ ⁻) to methanogenesis. The methanogenic toxicity of the NO_x⁻ compounds to anaerobic granular biofilms and municipal anaerobic digested sludge with two types of substrates, acetate and hydrogen, was studied. The inhibition was the severest when the NO_x⁻ compounds were still present in the media (exposure period). During this period, 95% or greater inhibition of methanogenesis was evident at the lowest concentrations of added NO₂ ⁻ tested (7.6–10.2 mg NO₂ ⁻-N l⁻¹) or 8.3–121 mg NO₃ ⁻-N l⁻¹ of added NO₃ ⁻, depending on substrate and inoculum source. The inhibition imparted by NO₃ ⁻ was not due directly to NO₃ ⁻ itself, but instead due to reduced intermediates (e.g., NO₂ ⁻) formed during the denitrification process. The toxicity of NO_x⁻ was found to be reversible after the exposure period. The recovery of activity was nearly complete at low added NO_x⁻ concentrations; whereas the recovery was only partial at high added NO_x⁻ concentrations. The recovery is attributed to the metabolism of the NO_x⁻ compounds. The assay substrate had a large impact on the rate of NO₂ ⁻ metabolism. Hydrogen reduced NO₂ ⁻ slowly such that NO₂ ⁻ accumulated more and as a result, the toxicity was greater compared to acetate as a substrate. The final methane yield was inversely proportional to the amount of NO_x⁻ compounds added indicating that they were the preferred electron acceptors compared to methanogenesis.     

The saturation of N cycling in Central Plains streams: <Superscript>15</Superscript>N experiments across a broad gradient of nitrate concentrations

We conducted ¹⁵NO₃⁻ stable isotope tracer releases in nine streams with varied intensities and types of human impacts in the upstream watershed to measure nitrate (NO₃⁻) cycling dynamics. Mean ambient NO₃⁻ concentrations of the streams ranged from 0.9 to 21,000 μg l⁻¹ NO₃⁻–N. Major N-transforming processes, including uptake, nitrification, and denitrification, all increased approximately two to three orders of magnitude along the same gradient. Despite increases in transformation rates, the efficiency with which stream biota utilized available NO₃⁻-decreased along the gradient of increasing NO₃⁻. Observed functional relationships of biological N transformations (uptake and nitrification) with NO₃⁻ concentration did not support a 1st order model and did not show signs of Michaelis–Menten type saturation. The empirical relationship was best described by a Efficiency Loss model, in which log-transformed rates (uptake and nitrification) increase with log-transformed nitrate concentration with a slope less than one. Denitrification increased linearly across the gradient of NO₃⁻ concentrations, but only accounted for ∼1% of total NO₃⁻ uptake. On average, 20% of stream water NO₃⁻ was lost to denitrification per km, but the percentage removed in most streams was <5% km⁻¹. Although the rate of cycling was greater in streams with larger NO₃⁻ concentrations, the relative proportion of NO₃⁻ retained per unit length of stream decreased as NO₃⁻ concentration increased. Due to the rapid rate of NO₃⁻ turnover, these streams have a great potential for short-term retention of N from the landscape, but the ability to remove N through denitrification is highly variable.     

The role of ion regulation in the control of the distribution of Gammarus tigrinus (Sexton) in salt-polluted rivers

Fluctuating salinities at different sites on the German salt-polluted rivers Werra and Weser were compared with extracellular ion levels of specimens of Gammarus tigrinus (Sexton; Amphipoda, Crustacea), collected at the same sites. G. tigrinus regulated haemolymph concentrations of inorganic anions (Cl⁻, SO²⁻ ₄, PO³⁻ ₄) and cations (Na⁺, K⁺, Mg²⁺, Ca²⁺) during fluctuations of salt pollution in the upper Weser. This capacity to regulate varying levels of salt pollution in the upper Weser, correlated well with the distribution of the brackish amphipods in this river ecosystem. G. tigrinus tolerated periods of Na⁺ and Cl⁻ stress (>380 mmol l⁻¹) without compensating these maxima by regulating extracellular Na⁺ and Cl⁻. However, during such bursts of Na⁺ and Cl⁻ stress in Werra and Weser, the ability to regulate extracellular [K⁺] at river water K⁺ stress of ≥6.0 mmol l⁻¹ may explain why this brackish species has been more successful in these rivers than its competitors like Gammarus pulex. The present investigation demonstrates that the water salinity affects the [NO⁻ ₃] in the haemolymph of G. tigrinus. With increasing hypo-osmotic stress the animals accumulate increasing amounts of NO⁻ ₃. A simultaneous increase in stream water [NO⁻ ₃] causes an additional accumulation of NO⁻ ₃ in the haemolymph. The high extent of accumulation indicates that active ion transport systems may be involved. The accumulation of NO⁻ ₃ in the haemolymph has low physiological consequences to G. tigrinus, but when hypo-osmotically stressed under anoxic conditions, nitrite formed by the reduction of nitrate may have an adverse affect on the metabolism of G. tigrinus. Accepted: 4 October 1999