Coupling of excitation and cessation of cyclois in Nitella: role of divalent cations

The effect of external divalent cation salt solutions upon the association of an action potential and cessation of cytoplasmic streaming in Nitella was studied. Nitella cells remained excitable when immersed in solutions of CaCl₂, MgCl₂, BaCl₂, and SrCl₂. Cessation of streaming coincident with excitation occurred in solutions of CaCl₂ or SrCl₂ but not in solutions of MgCl₂ or BaCl₂. In cells exposed to solutions containing mixtures of MgCl₂ and CaCl₂, or MgCl₂ and SrCl₂, it was the [Ca]/[Mg] or [Sr]/[Mg] which determined the effect of an action potential upon the rate of streaming, rather than the absolute concentrations Ca⁺⁺ or Sr⁺⁺. The implications of these data are discussed with respect to the structure involved in the generation of cytoplasmic streaming and the relation of streaming to other types of biological motion.     

Survival and death of Chara internodal cells in electrolyte solutions and calcium release from the cell wall

Abstract. Survival and death of Chara internodal cells were investigated in one of the alkali metal salts KCl, some of the alkali earth metal salts CaCl₂, Ca(NO₃)₂, MgCl₂, Mg(NO₃)₂, SrCl₂, Sr(NO₃)₂, BaCl₂ and Ba(NO₃)₂, potassium phosphate pH buffer solution (pH 7.0), Tris-maleate pH buffer solution (pH 7.0), HEPES (N-2-hydroxyethylpiperazine-N′-2-ethanesulphonic acid)-KOH (pH 7.0) pH buffer solution, calcium buffer solutions, and deionized water. Most of the internodal cells died within a day or a few days in KCl, MgCl₂, Mg(NO₃)₂, BaCl₂ and Ba(NO₃)₂ solutions of higher concentrations, calcium buffer solutions of pCa 6.0, 10.0 mol m^-3 potassium phosphate pH buffer solution and 10.0 mol m^-3 Trismaleate pH buffer solution. However, all of the internodal cells survived more than 10 d in deionized water, 80.0 mol m^-3 CaCl₂, 80.0 mol m^-3 Ca(NO₃)₂, 80.0 mol m^-3 SrCl₂, 80.0 mol m^-3 Sr(NO₃)₂ calcium buffer solutions of pCa 4.0 and pCa 5.0, and 10.0 mol m^-3 HEPES-KOH (pH 7.0) pH buffer solution. Addition of Ca²⁺ or Sr²⁺ to K⁺, Mg²⁺ and Ba²⁺ salt solutions increased the survival rates of the internodal cells. Calcium release from the internodal cell wall was measured in deionized water, KCl, NaCl, MgCl₂, CaCl₂, SrCl₂ and BaCl₂ solutions. Except in deionized water and CaCl₂ solution, most of the calcium binding to the cell wall was released within one or a few hours in respective electrolyte solutions. Thus, survival and death of the internodal cells in the electrolyte solutions tested were interpreted in terms of the calcium release from the cell wall and the cell membrane, and intrinsic ability of Sr²⁺ to maintain the cell membrane normal.     

Dissolved Inorganic Carbon Inventory and CO2Sequestration in Ureolytic Biocalcification Process with Bacillus Pasteurii

The generation and depletion of dissolved inorganic carbon (DIC) in a close-environment ureolytic biocalcification process by Bacillus pasteurii was evaluated. Three experimental sets, each containing 50 mM urea, were amended with either 50 mM Ca²⁺ before incubation (set–I) or 100 mM Ca²⁺ after 24-h incubation (set-II) or no Ca²⁺ addition (urea control).

Extent of ureolysis was maximum in urea control set (88%), followed by set–II (66.4%) and set–I (35.2%). Out of total DIC generated from microbial metabolism and ureolysis in set–I (277.6 mg/l) and set–II (464.9 mg/l), only about 54.1 mg/l and 180.1 mg/l was precipitated as CaCO₃, whereas 189.3 mg/l and 231.3 mg/l DIC escaped into headspace, respectively. Increased time separation between ureolysis and calcification steps in set–II and higher dosage of Ca²⁺ resulted in synergistic improvement in DIC capture. In a reusability test, the spent supernatant from set–II could precipitate additional amount CaCO₃from CO₂saturated water_,which was twice as much as that of the fresh media control.     

Bacterial Calcium Carbonate Precipitation in Cave Environments: A Function of Calcium Homeostasis

To determine if microbial species play an active role in the development of calcium carbonate (CaCO ₃ ) deposits (speleothems) in cave environments, we isolated 51 culturable bacteria from a coralloid speleothem and tested their ability to dissolve and precipitate CaCO ₃ . The majority of these isolates could precipitate CaCO ₃ minerals; scanning electron microscopy and X-ray diffractrometry demonstrated that aragonite, calcite and vaterite were produced in this process. Due to the inability of dead cells to precipitate these minerals, this suggested that calcification requires metabolic activity. Given growth of these species on calcium acetate, but the toxicity of Ca ²⁺ ions to bacteria, we created a loss-of-function gene knock-out in the Ca ²⁺ ion efflux protein ChaA. The loss of this protein inhibited growth on media containing calcium, suggesting that the need to remove Ca ²⁺ ions from the cell may drive calcification. With no carbonate in the media used in the calcification studies, we used stable isotope probing with C ¹³ O ₂ to determine whether atmospheric CO ₂ could be the source of these ions. The resultant crystals were significantly enriched in this heavy isotope, suggesting that extracellular CO ₂ does indeed contribute to the mineral structure. The physiological adaptation of removing toxic Ca ²⁺ ions by calcification, while useful in numerous environments, would be particularly beneficial to bacteria in Ca ²⁺ -rich cave environments. Such activity may also create the initial crystal nucleation sites that contribute to the formation of secondary CaCO ₃ deposits within caves.     

Ca2+ effects on ethylene, carbon dioxide and 1-aminocyclopropane-1-carboxylic acid synthase activity

The response of pericarp disks from ripening tomato (Lycopersicon esculentum Mill. cv. Traveler‘76) to CaCl₂, additions was studied to determine the effect of Ca²⁺ on ethylene and CO₂ production. Application of 5 mM CaCl₂ resulted in a 2, 20, 33, 39, and 50% increase in ethylene production in disks obtained from preclimacteric minimum, climacteric rise, climacteric peak, one, and two days postclimacteric fruit, respectively. CaCl₂ concentrations of 10 and 50 mM gave no additional stimulation of ethylene production; CO₂ production at 5 mM CaCl₂ was not different from controls, but is increased at 10 and 50mM CaCl₂. CaCl₂ also increased ethylene production in disks treated with 1-aminocyclopropane-1-carboxylic acid (ACC) or aminoethoxy-vinylglycine. Chloride salts of K⁺, Na⁺, Mg²⁺, Sr²⁺ and La³⁺ did not stimulate ethylene production. SrCl₂ stimulated ethylene production to a lesser degree than CaCl₂. Disks from potato (Solanum tuberosum L. cv. Katahdin) tubers produced greater quantities of ethylene and ACC when 5 mM CaCl₂ was included in the incubation medium (K. B. Evensen, 1983. Physiol. Plant. 60:125–128). Ca²⁺-treated disks had more than three times as much ACC synthase activity as control disks after 18 to 24 h incubation, when ethylene and ACC were maximal. The apparent K_m for S-adenosylmethionine was 13 μM at 29°C, pH 8.0 in extracts from both Ca²⁺-treated and control disks. Inclusion of 1 to 50 mM CaCl₂ in the assay medium did not significantly affect enzyme activity. ACC synthase extracted from control and Ca²⁺-treated disks had a pH optimum of 8.5 and an apparent molecular weight of 72 kdalton, estimated by gel filtration. It is likely that the presence of Ca²⁺ in the buffer allows greater synthesis of ACC synthase as part of the wound-healing response in potato, while in tomato the predominant effect is on membrane stabilization.     

Induction of Calcium Carbonate by Bacillus cereus

The purpose of this research was to study how the bacteria Bacillus cereus (DCB1) utilizes calcium ions in a culture medium with carbon dioxide (CO₂) to yield calcium carbonate (CaCO₃). The bacteria strain DCB1 was a dominant strain isolated from dolomitic surfaces in areas of Karst topographies. The experimental method was as follows: a modified beef extract-peptone medium (beef extract 3.0 g, peptone 10 g, NaCl 5.0 g, CaCl₂ 2.0 g, glass powder 2.0 g, distilled water 1 L, and a pH between 6.5 and 7.5) was inoculated with B. cereus to attempt to induce the synthesis of CaCO₃. The sample was then processed by centrifugation every 24 h during the 7-day cultivation period. The pH, carbonic anhydrase (CA) activity, and the concentrations of both HCO^- ₃ and Ca²⁺ in the supernatant fluid were measured. Subsequently, precipitation in the culture medium was analyzed to confirm, or otherwise, the presence and if present, the formation, of CaCO₃. Methods used included X-ray diffraction (XRD), Scanning Electron Microscopy (SEM), Transmission Electron Microscopy (TEM), and Energy Dispersive Spectroscopy (EDS). Meanwhile, the carbon source in the carbonate was classified by its isotope composition. Results showed that B. cereus can improve its pH value in this culture medium; concentrations of HCO^- ₃ and Ca²⁺ showed a significant decline over the duration of the cultivation period. CA activity reached its maximum during the second day; XRD, SEM, TEM, and isotope analysis all revealed the presence of CaCO₃ as a precipitate. Additionally, these results did not occur in an aseptic control group: no detectable level of CaCO₃ was produced therein. In conclusion: B. cereus can metabolize active materials, such as secretase, by its own growth and metabolism, and can either utilize atmospheric CO₂, or respire, to induce CaCO₃ production. Experimental evidence is offered for a concomitant CO₂ reduction and CaCO₃ induction by microorganisms.     

Microbial populations, ammonification and nitrification in soil treated with urea and inorganic salts

Soil fertilization with urea at rates of 0.2 and 0.5 mg N/g soil was toxic for total counts of bacteria and fungi except with cellulolytic fungi where growth was promoted by addition of urea after 90-d incubation. Also, the population numbers of both bacteria and fungi were significantly decreased when soil was amended with CaCl₂ and K₂SO₄ applied at two levels (50 and 100 μmol/g soil). Some alleviation of the toxic effect of either urea or the inorganic salts was observed when they were applied in combination. Fungal species composition was found to be affected in the treated soil. The most tolerant fungi wereAlternaria alternata, Aspergillus flavus, A. fumigatus, A. niger, A. terreus, Eurotium amstelodami, E. chevalieri, Nectria hœmatococca, Pœcilomyces variotii andStachybotrys chartarum. Other species of fungi were either sensitive to all treatments or sensitive to some and tolerant to others. Ammonium nitrogen was found to be more accumulated in soil treated with urea mixed with inorganic salts compared with soil treated only with urea whereas NO ₃ ⁻ -N (and NO ₂ ⁻ -N) was decreased. The overall effect of the addition of inorganic salts on total mineralized nitrogen, however was promotive. Soil pH was increased in ureatreated soil but was depressed by application of CaCl₂ or K₂SO₄ to values lower than that of untreated soil. The results may be of agronomical interest in overcoming problems encountered with urea application as N fertilizer.     

An introduction to the biogeochemical cycling of calcium and substitutive strontium in living coral reef mesocosms

The coral reef mesocosms designed by the Smithsonian Institution's Dr. Walter Adey, his Marine System Laboratory personnel, and staff members of the Pittsburgh Aqua-Zoo simulate most of the physical, chemical, and biological parameters found in natural Caribbean coral reefs. After developing the mesocosm in Pittsburgh, an evaluation and comparison between natural reef seawater sources and closed mesocosm seawater conditions indicated that an additional parameter should be investigated. It was hypothesized that, given time, the aragonite- and calcite (CaCO₃ crystal forms)-producing organisms in the closed mesocosms could deplete the seawater of available Ca²⁺ and substitutive Sr²⁺. Atomic absorption spectrophotometry was utilized to determine concentrations in the seawater over time. Results showed a substantial reduction in dissolved Ca and Sr in the mesocosm after approximately two years. Dissolved aragonitic Halimeda algae parts were put into the system for replacive purposes. In terms of the biogeochemical cycling of Ca²⁺ and Sr²⁺, the coral reef mesocosm organisms behaved similarly to natural reefs, which have a constant supply of dissolved Ca²⁺ and Sr²⁺. Further research utilizing radiolabeled sources of Ca²⁺, Sr²⁺, and Mg²⁺, in conjunction with in vivo scanning electron microscopy (SEM) and growth increment studies, are recommended for determining the exact biogeochemical pathways for these elements in coral reefs, and to quantify growth parameters. © 1993 Wiley-Liss, Inc.     

Role of calcium in the initiation of fast axonal transport of protein: Effects of divalent cations

Fast axonal transport of [³H]protein has been examined in bullfrog primary afferent neurons incubated in media supplemented with divalent cations that can act as agonists or antagonists of calcium ions. Incubation in calcium-free medium (CFM) had no effect on the rate of transport, but reduced the amount of transported [³H]protein by 40–60% relative to transport in the contralateral preparation maintained in normal medium. Preparations incubated in CFM supplemented with 1.8 mM SrCl₂ (equimolar to the CaCl₂ concentration in normal medium) carried out transport at control levels. Incubation conditions in which primary afferent somata were exposed to the Sr²⁺-medium while nerve trunks were maintained in CFM also supported normal transport. By contrast, selective exposure of nerve trunks to Sr²⁺-medium, and somata to CFM resulted in a reduced level of transport similar to that observed when the whole preparation was incubated in CFM. The depression of transport resulting from incubation in CFM was shown to be reversible when preparations were transferred from CFM to either Sr²⁺-supplemented CFM or to normal medium. By contrast to the effects of Sr²⁺, Ba²⁺ (up to 18 mM) did not substitute for Ca²⁺ in the transport process. When normal medium was supplemented with calciumantagonist cations, the amount of transport was depressed (Co²⁺ > Mn²⁺ >> Mg²⁺), with no concomitant effect on the rate of transport. Results of studies with Co²⁺, as well as those with Sr²⁺, suggest that a major locus of action of these cations is within the neuronal soma at a step subsequent to protein synthesis, and prior to the onset of protein translocation via the transport system. Thus, it is inferred that these divalent cations affect a calcium-dependent step that occurs during the initiation phase of fast axonal transport.     

Stable isotope fractionation of strontium in coccolithophore calcite: Influence of temperature and carbonate chemistry

Marine calcifying eukaryotic phytoplankton (coccolithophores) is a major contributor to the pelagic production of CaCO₃ and plays an important role in the biogeochemical cycles of C, Ca and other divalent cations present in the crystal structure of calcite. The geochemical signature of coccolithophore calcite is used as palaeoproxy to reconstruct past environmental conditions and to understand the underlying physiological mechanisms (vital effects) and precipitation kinetics. Here, we present the stable Sr isotope fractionation between seawater and calcite (Δ^88/86Sr) of laboratory cultured coccolithophores in individual dependence of temperature and seawater carbonate chemistry. Coccolithophores were cultured within a temperature and a pCO₂ range from 10 to 25°C and from 175 to 1,240 μatm, respectively. Both environmental drivers induced a significant linear increase in coccolith stable Sr isotope fractionation. The temperature correlation at constant pCO₂ for Emiliania huxleyi and Coccolithus braarudii is expressed as Δ^88/86Sr = ?7.611 × 10^?3 T + 0.0061. The relation of Δ^88/86Sr to pCO₂ was tested in Emiliania huxleyi at 10 and 20°C and resulted in Δ^88/86Sr = ?5.394 × 10^?5 pCO₂ – 0.0920 and Δ^88/86Sr = ?5.742 × 10^?5 pCO₂ – 0.1351, respectively. No consistent relationship was found between coccolith Δ^88/86Sr and cellular physiology impeding a direct application of fossil coccolith Δ^88/86Sr as coccolithophore productivity proxy. An overall significant correlation was detected between the elemental distribution coefficient (D_Sr) and Δ^88/86Sr similar to inorganic calcite with a physiologically induced offset. Our observations indicate (i) that temperature and pCO₂ induce specific effects on coccolith Δ^88/86Sr values and (ii) that strontium elemental ratios and stable isotope fractionation are mainly controlled by precipitation kinetics when embedded into the crystal lattice and subject to vital effects during the transmembrane transport from seawater to the site of calcification. These results provide an important step to develop a coccolith Δ^88/86Sr palaeoproxy complementing the existing toolbox of palaeoceanography.     

Luminescence enhancement of (Sr1–xMx)2SiO4:Eu2+ phosphors with M (Ca2+/Zn2+) partial substitution for white light‐emitting diodes

Eu²⁺‐doped Sr₂SiO₄ phosphor with Ca²⁺/Zn²⁺ substitution, (Sr_1–xM_x)₂SiO₄:Eu²⁺ (M = Ca, Zn), was prepared using a high‐temperature solid‐state reaction method. The structure and luminescence properties of Ca²⁺/Zn²⁺ partially substituted Sr₂SiO₄:Eu²⁺ phosphors were investigated in detail. With Ca²⁺ or Zn²⁺ added to the silicate host, the crystal phase could be transformed between the α‐form and the β‐form of the Sr₂SiO₄ structure. Under UV excitation at 367 nm, all samples exhibit a broad band emission from 420 to 680 nm due to the 4f⁶5d¹ → 4f⁷ transition of Eu²⁺ ions. The broad emission band consists of two peaks at 482 and 547 nm, which correspond to Eu²⁺ ions occupying the ten‐fold oxygen‐coordinated Sr.(I) site and the nine‐fold oxygen‐coordinated Sr.(II) site, respectively. The luminescence properties, including the intensity and lifetime of Sr₂SiO₄:Eu²⁺ phosphors, improved remarkably on Ca²⁺/Zn²⁺ addition, and promote its application in white light‐emitting diodes. Copyright © 2016 John Wiley & Sons, Ltd.     

Cation‐tunable blue phosphor Ca2PO4Cl:Eu2+: enhancive emission and site occupancy

A series of blue phosphors Ca_1.98–xM_xPO₄Cl:0.02Eu²⁺ (M = Mg and Sr) with different values of x were synthesized using a high‐temperature solid‐state reaction. X‐Ray diffraction and photoluminescence measurements were used to study the phase structure and luminescence properties. Ca₂PO₄Cl:0.02Eu²⁺ exhibits a tunable emission intensity and color due to the incorporation of Sr²⁺ or Mg²⁺. The incorporation of Sr²⁺ reduces the luminescence intensity and results in a slight red shift in the emission band. The incorporation of Mg²⁺ results in enhanced emission and a clear blue shift in the emission band along with a tunable chromatic coordination. Under excitation at λ = 334 nm, the emission intensity of the Mg²⁺‐doped Ca₂PO₄Cl:0.02Eu²⁺ is found to be 250% that of Ca₂PO₄Cl:0.02Eu²⁺. The luminescence behaviors of the as‐synthesized phosphors are discussed according to the host crystal structure and site occupancy of Eu²⁺. The results indicate that Mg²⁺‐doped Ca₂PO₄Cl:Eu²⁺ is more applicable as a near‐UV‐convertible blue phosphor for white light‐emitting diodes. Copyright © 2015 John Wiley & Sons, Ltd.     

ATP-dependent strontium uptake by basolateral membrane vesicles from rat renal cortex in the absence or presence of calcium

ATP-dependent Sr²⁺ transport was examined in vitro using basolateral membrane (BLM) vesicles isolated from rat renal cortex to clarify the discrimination mechanisms between strontium (Sr) and calcium (Ca) in renal tubules during reabsorption. ATP-dependent Sr²⁺ uptake and Ca²⁺ uptake were observed in renal BLM vesicles and were inhibited by vanadate. Hill plots indicate similar kinetic behavior for Ca²⁺ and Sr²⁺ uptake. The apparentK _m andV _max of ATP-dependent Sr²⁺ uptake were both higher than those for Ca²⁺ uptake. ATP-dependent Sr²⁺ uptake by BLM vesicles diminished in the presence of 0.1 μM Ca²⁺ and was more markedly inhibited by 1 μM Ca²⁺. Hill plots of Sr²⁺ uptake data with and without 0.1 μM Ca²⁺ showed that the cooperative behavior of Sr²⁺ uptake was not changed by Ca²⁺. In the presence of 0.1 μM Ca²⁺, the affinity of the transport system for Sr²⁺ and the velocity of Sr²⁺ uptake in the BLM were both decreased. However, the rate of Ca²⁺ uptake was not diminished by Sr²⁺ concentrations of <1.6 μM. These results suggest that Ca²⁺ is preferentially transported in the renal cortex BLM when Ca²⁺ and Sr²⁺ are present at the same time.     

Enhancement of yeast ethanol tolerance by calcium and magnesium

Ethanol-induced changes of CO₂ production were compared in three strains ofSaccharomyces cerevisiœ. CaCl₂ and MgCl₂ exerted protective effects against the action of ethanol. Optimal concentrations ensuring maximum of CO₂ production at 10% (V/V) of ethanol under non-growing conditions were 3 mmol/L Ca²⁺ and 2 mmol/L Mg²⁺. Yeast growth with and without ethanol addition was stimulated by Mg²⁺ more than by Ca²⁺ during fermentation, whereas ethanol production was more efificient when both Ca²⁺ and Mg²⁺ were added.     

The improvement of glucose/xylose fermentation by Clostridium acetobutylicum using calcium carbonate

Batch fermentation of 60g/l glucose/xylose mixture by Clostridium acetobutylicum ATCC 824 was investigated on complex culture medium. Different proportions of mixtures, ranged between 10 and 50g of each sugar/l, were fermented during pH control at 4.8 (optimum pH for solventogenesis) or during CaCO₃ addition. Using xylose-pregrown cells and pH control, an important amount of xylose was left over at the end of the fermentation when the glucose concentration was higher than that of xylose. The addition of 10g of CaCO₃/l (to prevent the pH dropping below 4.8) increased xylose uptake: a substantial decrease of residual xylose was observed when xylose-pregrown cells as well as glucose-pregrown cells were used as inoculum for all the mixture proportions studied. MgCO₃ (Mg²⁺-containing compound) and CaCl₂ (Ca²⁺-containing compound) reduced residual xylose only during pH control at 4.8 by NaOH addition. As butanol is the major limiting factor of xylose uptake in C. acetobutylicum, fermentations were carried out with or without CaCO₃ in butanol-containing media or in iron deficient media (under iron limitation, butanol synthesis occurred early and could inhibit xylose uptake). Results showed that an excess of CaCOCaCO₃ could increase butanol tolerance which resulted in an increase in xylose utilization. This positive effect seem to be specific to Ca²⁺- or Mg²⁺-containing compounds, going beyond the buffering effect of carbonate.     

Enhancement of salt responses in frog gustatory nerve by removal of Ca2+ from the receptor membrane treated with 1-anilinonaphthalene-8-sulfonate

Summary The frog tongue was incubated in 1-anilinonaphthalene-8-sulfonate (ANS) solution and the responses of the glossopharyngeal nerve to various chemical stimuli were measured after the ANS solution was washed out. The responses to galactose, quinine and distilled water were unchanged by the ANS treatment. On the other hand, the responses to the salts, except for CaCl₂, were enhanced in greater or lesser degree after the ANS treatment. The order of relative magnitude of the enhanced response to 100mm salts of monovalent cations was Na⁺>NH ₄ ⁺ >K⁺>Li⁺, while that before the treatment was NH ₄ ⁺ >K⁺>Na⁺>Li⁺. The enhancement of the salt responses was also observed after the tongue was treated with 6-p-toluidinonaphthalene-2-sulfonate or 1,2-cyclohexanediaminetetraacetic acid solution.The enhanced responses to the salts were suppressed to the original level before the ANS treatment by addition of CaCl₂ or SrCl₂. The suppression curve satisfied the Langmuir adsorption isotherm when the suppression was postulated to be responsible for the binding of Ca²⁺ or Sr²⁺ to the receptor membrane treated with ANS. The apparent binding constants for Ca²⁺ and Sr²⁺ in the presence of 100mm NaCl were obtained to be 1.2×10⁴ m ^–1 and 6.7×10³ m ^–1, respectively.The ANS treatment modified the temperature dependence of the salt responses. For example, 100mm KCl solution of low temperature induced a large response after the ANS treatment, while that of 20°C induced only small response.It was concluded that the removal of Ca²⁺ from the gustatory receptor membrane in the frog, which was brought about by the ANS treatment, led to the enhancement of the salt responses. The mechanism on the enhancement of the salt response by the Ca²⁺ removal was discussed.     

Tunable white light emission from single‐phased Li2SrSiO4:Dy3+ phosphors by co‐doping with Eu3+

A series of single‐phase full‐color emitting Li₂Sr_1−x−ySiO₄:xDy³⁺,yEu³⁺ phosphors were synthesized by solid‐state reaction and characterized by X‐ray diffraction and photoluminescence analyses. The samples showed emission peaks at 488 nm (blue), 572 nm (yellow), 592 nm (orange) and 617 nm (red) under 393 nm excitation. The photoluminescence excitation spectra, comprising the Eu–O charge transfer band and 4f–4f transition bands of Dy³⁺ and Eu³⁺, range from 200 to 500 nm. The Commission Internationale de I'Eclairage chromaticity coordinates for Li₂Sr_0.98−xSiO₄:0.02Dy³⁺,xEu³⁺ phosphors were simulated. By manipulating Eu³⁺ and Dy³⁺ concentrations, the color points of Li₂Sr_1−x−ySiO₄:xDy³⁺,yEu³⁺ were tuned from the greenish‐white region to white light and eventually to reddish‐white region, demonstrating that a tunable white light can be obtained by Li₂Sr_1−x−ySiO₄:xDy³⁺,yEu³⁺ phosphors. Li₂Sr_0.98−xSiO₄:0.02Dy³⁺, xEu³⁺ can serve as a white‐light‐emitting phosphor for phosphor‐converted light‐emitting diode. Copyright © 2014 John Wiley & Sons, Ltd.     

Impact of temperature on Na2Sr(PO4)F:Eu3+ phosphor

In this article, we report the synthesis of Na₂Sr_1‐x(PO₄)F:Eu_x phosphor via a combustion method. The influence of different annealing temperatures on the photoluminescence properties was investigated. The phosphor was excited at both 254 and 393 nm. Na₂Sr_1‐x(PO₄)F:Eu_x³⁺ phosphors emit strong orange and red color at 593 and 612 nm, respectively, under both excitation wavelengths. Na₂Sr_1‐x(PO₄)F:Eu_x³⁺ phosphors annealed at 1050°C showed stronger emission intensity compared with 600, 900 and 1200°C. Moreover, Na₂Sr_1‐x(PO₄)F:Eu_x³⁺ phosphor was found to be more intense when compared with commercial Y₂O₃:Eu³⁺ phosphor. Copyright © 2013 John Wiley & Sons, Ltd.     

Calcium carbonate formation by Enteromorpha nana algae in a hypersaline volcanic crater lake

On the black basaltic rock surfaces in shallow water around the margin of Lake Gnotuk, and for several meters above the present lake, there is a thick white coating of aragonite marl. The water in the lake is supersaturated with CaCO₃.From close observation and experimental work, it is evident that the marl is produced by the alga Entermorpha nana which lives in the shallow lake water and grows attached to the basalt. The general mechanism of CaCO₃ precipitation by aquatic plants is outlined, and in Enteromorpha nana it can be demonstrated that the closed tubular thallus absorbs HCO-₃ from the outside water and secretes CO²-₃ inside the tube. This secretion of CO²-₃ greatly increases the ionic product of [Ca²⁺] [CO₂-₃] in the water inside the thallus and leads to the precipitation of aragonite and its accumulation at the base of the tube.     

The impacts of a watershed CaCO3 treatment on stream and wetland biogeochemistry in the Adirondack Mountains

Temporal and longitudinal variations in the chemistry of two tributary streams of Woods Lake in the Adirondack Mountains of New York were monitored before and after a watershed CaCO₃ application. One subcatchment of the lake had a large beaver pond and wetland at its headwaters, while the second was free-flowing. Treatment of both subcatchments with CaCO₃ resulted in an immediate increase in acid neutralizing capacity (ANC) associated with Ca²⁺ release. The extent and duration of the response to the treatment were greater in the wetland-impacted stream. Aluminum was retained and complexed with organic solutes generated within the beaver-pond. In the free-flowing stream, NO ₃ ^– concentration increased significantly after the manipulation; this pattern was not evident in the wetland-impacted stream. Net retention of SOkinf4/sup2– was evident in the beaver pond prior to and following treatment, and this response was enhanced after the watershed liming. Comparisons of beaver pond inlet/outlet concentrations, mass balance calculations, and in-pond profiles of chemical parameters revealed patterns of retention of SO ₄ ^2– , NO ₃ ^– and Al, and release of Fe²⁺, dissolved organic carbon (DOC) and NH ₄ ⁺ in the wetland during the summer before CaCO₃ treatment. Post-treatment releases of Ca²⁺ from the near-sediment zone in the beaver pond corresponded to anoxic periods in mid- to late-summer and under ice in winter. These findings demonstrate the importance of increased microbial processing of organic matter, along with high partial pressure Of CO₂ (Pco₂) in facilitating the dissolution of the applied CaCO₃. Dissolved silica (H₄SiO₄) was retained in the wetland during the summer prior to treatment but was released after the manipulation. This phenomenon may reflect the dissolution of diatom frustules or silicate minerals in the wetland at higher pH and DOC concentrations. Within two years of the CaCO₃ treatment 60% of the CaCO₃ applied to the beaver pond and surrounding wetland was dissolved and transported from the pond, in contrast to only 2.2% of the CaCO₃ applied to the upland subcatchment draining into the wetland. These results, coupled with high quantities of exchangeable Ca²⁺ found in sediments and onSphagnums mosses in the pond, demonstrate the importance of hydrologic source areas and wetlands in facilitating the dissolution of added CaCO₃ and in regulating the production of chemical species important in ANC generation.