Response-velocity of chloride absorption by barley roots to oligomycin

Chloride absorption by excised barley roots is significantlyinhibited within the first 2 min of incubation in oligomycin.A steady inhibited absorption rate is attained in the presenceof oligomycin after 10 min (Received February 18, 1970; )     

Responses of periphyton to changes in current velocity, suspended sediment and phosphorus concentration

SUMMARY.

• 1 Research was performed in laboratory streams to evaluate periphytic biomass accrual, export, and community composition over a range of limiting nutrient (phosphorus) concentrations with variable velocity, and suspended sediment addition, in comparison to constant velocity and no suspended sediment. In fixed-velocity treatments, velocity increase to 60 cm s^?1 significantly enhanced biomass accrual, but further increase resulted in substantial biomass reduction. Average biomass loss rates did not change significantly over a velocity range of 10–80 cm s^?1. Diatoms were favoured at relatively high velocities and low phosphorus concentrations, whereas the blue-green Phormidium tended to dominate at higher SRP concentrations and the green Mougeotia seemed to prefer lower velocities.
• 2 Sudden increases in velocity raised instantaneous loss rates by an order of magnitude or more, but these high rates persisted only briefly. As a result, marked biomass reductions were not apparent a day after the velocity change. Dominance change from filamentous green or blue-green to diatoms immediately after the increase was reversed within 2 days. Loss rate increases due to solids addition were much smaller than those accompanying velocity increase, but simultaneous velocity elevation and solids addition produced instantaneous loss rates approximately double those with velocity increase alone.
• 3 The experiments demonstrated that an elevation in velocity, above that to which algae were accustomed, led to increased loss rates and temporarily reduced biomass. However, recolonization and growth after biomass reduction were apparently rapid. Substantial export of periphyton following solids addition required erosion of the protective boundary layer accompanied by a velocity increase. These results arc applicable to understanding the response of lotic periphytic algae to elevated, turbid storm discharges and similar runoff or high-flow events.
• 4 Areal uptake rates of P by algae growing in the laboratory streams increased with soluble reactive phosphorus (SRP) concentration, up to approximately 15 μg I^?1 in overlying water. They also increased above 35 cm s ^?1. Overall, uptake rate seemed to vary inversely with biomass. The ralio of areal uptake rate/biomass was significantly less where mean biomass was 411±6 mg chl a m^?2 compared to 223±17 mg chl a m^?2.
• 5 The results suggested that although nutrient uptake is primarily a surface phenomenon, diffusion to interior cells can also determine the responses of attached communities. Both diffusion and uptake rate were stimulated by increasing nutrient concentration and velocity up to certain levels, but became limited by biofilm thickness and scouring.

     

Sodium Recirculation and Loss from Phaseolus vulgaris L.

In a split-root experiment, ²²Na was supplied to Phaseolus vulgarisL. roots emerging from the stem, 2.5 cm above the main roots.Sodium exported from these upper roots was translocated a shortdistance upward in the stem and downward to the main roots.Most of the ²²Na arriving in the main roots was lost to themedium. Sodium loss from P. vulgaris roots into KCI or NaCl was similarand was not affected by oligomycin. The results confirm a previous hypothesis regarding the mechanismof sodium exclusion from the tops of sodium non-accumulatorplants. Phaseolus vulgaris L., bean, sodium transport     

The Effect of the Roots on Calcium Ascent in Bean Stems

Bean roots enhance calcium translocation in the stems by supplyingto the ascending sap other previously accumulated cations. Theseions apparently compete with calcium for binding sites in thestem.     

Proton-Chloride Symport in Barley Roots

An increase in the acidity of the incubation medium from pH6 5 to pH 4.0 increased Cl- flux into ATP-depleted Hordeum vulgareL roots more than three times This pH-dependent Cl^– fluxwas inhibited by p-chloromercuriphenyl sulphonic acid. The effectof pH on Cl- influx was eliminated when the pH gradient wasdissipated by addition of salts of permeable weak acids, andin K-loaded roots in the presence of a protonophore togetherwith valinomycin The results support the assumption that a H⁺-Cl^–symportsystem is present in barley root cells Hordeum vulgare L., barley, excised roots, ion transport, proton-chloride symport     

Some Aspects of Chloride Absorption by Bean Leaf Tissue

Rates of active chloride absorption by thin bean leaf slicesfrom 0.1 mM aqueous potassium chloride are about one-tenth ofthe rates for monovalent cation absorption by such slices andabout one-sixth of chloride absorption rates by excised beanroots. In the 2.0–5.0 mM concentration range chlorideabsorption rates of bean leaf and root tissues do not differmuch and are similar to those of monovalent cation absorptionrates.     

Sodium fluxes in corn roots: comparison to Cl and K fluxes, and to Na-fluxes in barley

Abstract. Carbonylcyanide, m -chlorophenyl hydra-zone (CCCP) decreased the ATP content of barley and corn roots by 80% within 5 min. The protonophore inhibited K and Cl absorption by largely unvacuolated root tips, and vacuolated root segments of barley and corn. The protonophore also inhibited Na absorption by root segments and Na extrusion by root tips of barley; it did not affect these Na fluxes in corn root tips and segments, and Na Influx in barley root tips. It was concluded that corn roots lack a metabolic mechanism for Na extrusion from the cytoplasm to the external solution or vacuole, which is functional in barley roots.