Coulometric determination of dissolved oxygen in water

The oxygen content of air-saturated distilled water has been determined at between 10 and 40 degrees by using a controlled-potential coulometric method based on an earlier published method for the iodometric determination of nitrite. The maximum error for the determinations was +/- 0.3% over the whole range, and the time of analysis about 3 min. An equation is given for the solubility in the measured range, and some thermodynamic functions are calculated.     

Studies on the determination of dissolved oxygen in water

Studies on the decomposition rates of the Mn(III) complex of cyclohexanediaminetetra-acetate (DCTA) in light and in darkness have shown that this complex is more stable than the one derived from ethylenediaminetetra-acetate. The optimum pH range for the determination of dissolved oxygen by means of the Mn(III)-DCTA complex is found to be between 3 and 4. The absorbance of this complex is independent of the amount of DCTA used (in the range 0.2–1.0 g) with water samples containing a maximum of 3.2 ppm of dissolved oxygen. Significant interferences are caused by the presence of CO²⁻₃, HCO⁻₃, S₂O²⁻₃, PO³⁻₄, I⁻, NO⁻₂, SO²⁻₃, Ca²⁺, Fe²⁺ and Fe³⁺ at 500 times the oxygen concentration.     

Titrimetric determination of dissolved oxygen in waste water

Winkler's procedure for the determination of dissolved oxygen has been modified to cope with substantial amounts of oxidizing or reducing substances in the samples. The manganese(III) is treated with an excess of hydroquinone, the unconsumed part of which is then titrated with standard ceric sulphate solution. A blank determination is also carried out, in which the order of addition of reagents is reversed so that the solution is always acidic, to allow for the interfering substances present. Results obtained by using this modified procedure on clean samples are in good agreement with results obtained by the usual Winkler method.     

A highly accurate method for determination of dissolved oxygen: Gravimetric Winkler method

A high-accuracy Winkler titration method has been developed for determination of dissolved oxygen concentration. Careful analysis of uncertainty sources relevant to the Winkler method was carried out and the method was optimized for minimizing all uncertainty sources as far as practical. The most important improvements were: gravimetric measurement of all solutions, pre-titration to minimize the effect of iodine volatilization, accurate amperometric end point detection and careful accounting for dissolved oxygen in the reagents. As a result, the developed method is possibly the most accurate method of determination of dissolved oxygen available. Depending on measurement conditions and on the dissolved oxygen concentration the combined standard uncertainties of the method are in the range of 0.012–0.018 mg dm⁻³ corresponding to the k = 2 expanded uncertainty in the range of 0.023–0.035 mg dm⁻³ (0.27–0.38%, relative). This development enables more accurate calibration of electrochemical and optical dissolved oxygen sensors for routine analysis than has been possible before.     

A reverse-flow injection analysis method for the determination of dissolved oxygen in fresh and marine waters

A reverse flow injection method (rFIA) based on the Winkler titration chemistry, is reported for the determination of dissolved oxygen (DO) in natural waters. Manganese(II) sulfate is injected into a continuously flowing stream of sample and subsequently merges with a reagent stream of sodium hydroxide and sodium iodide. Manganese(II) hydroxide that is formed reacts with DO in the sample to form an oxidized manganese hydroxyoxide floc. Addition of 10% sulfuric acid dissolves this floc, and under acidic conditions, the triiodide ion formed is detected by photometry in a flow through cell at a wavelength of 440 nm. The method is rapid (48 measurements per h), repeatable (R.S.D. ca. 3%, n=3), and has a calculated detection limit of 0.25 mg l⁻¹ (P=0.001). No interference from nitrite or ferrous ions was observed at concentrations typically found in natural waters. The method has been successfully applied to on-line measurement of DO in sediment respiration reactors.     

Indirect determination of oxygen dissolved in water by atomic absorption spectrometry

Summary Indirect Determination of Oxygen Dissolved in Water by Atomic Absorption Spectrometry O₂ dissolved in aqueous medium reacts quantitatively with thallium metal according to O₂+4 Tl+2 H₂O 4 Tl⁺+4 OH^–. The reaction takes place in a glass column filled up with small pieces of sheet metal. The Tl⁺ formed is measured by atomic absorption spectrometry. We study the influence of several factors (pH, temperature, salinity of the water). The results obtained from a statistical sample were compared with those provided by the amperometric method for direct determination of dissolved O₂ and we found a high degree of consistency between them.     

A semi-automatic alkaline peroxodisulphate method for the routine determination of total dissolved nitrogen in sea water

Nydahl's method for the determination of dissolved organic nitrogen (DON) in distilled water has been modified for the determination of total dissolved nitrogen (TDN) in sea water. Samples (9 cm³) are digested batch-wise with alkaline potassium peroxodisulphate solution. An improved buffering system permits the automatic measurement of the nitrate formed, and allows the analysis of 50–80 samples per day. DON may be determined as the difference between TDN and the sum of inorganic nitrogen species. The standard deviation of TDN determinations is 0.7 μg N dm^-3 at about 15 μg TDN dm^-3. The method is applied to a range of samples including tanker ballast water, oil platform production water, and zooplankton.     

Design and evaluation of an electrochemical sensor for determination of dissolved oxygen in water

A voltammetric cell with a graphite-paste cathode and silver-wire anode was designed for dissolved oxygen determinations in water. Its most important features were evaluated in laboratory and field studies. Several advantages such as higher sensitivity, wider linear response interval, negligible interference due to carbon dioxide, and shorter response time, besides its low cost and simple construction, were found when it was compared with sensors having a platinum cathode.     

A simple chemiluminescence method for determination of chemical oxygen demand values in water

In this paper, a low cost chemiluminescence detector with a photodiode instead of photo-multiplier tube (PMT) was developed for environmental monitoring of water quality. Based on the chemiluminescent reaction of luminol-H₂O₂-Cr³⁺ system, light emission caused by luminol-H₂O₂-Cr³⁺ system was detected by the photodiode, and its intensity caused by the appearance of Cr³⁺ after samples digestion was proportional to the chemical oxygen demand (COD). Effects for COD determining such as pH, concentrations, interference, and digestion procedures were investigated. The experimental results show that this suggested method uses an instrument that is simpler and cheaper than the previous ones used for the same purpose. The data obtained by the present method were fairly in good agreement with those obtained by the standard reflux titrimetric method. It has been applied to determine real samples with satisfactory results.     

Microdetermination of dissolved oxygen in water by a rapid spectrophotometric method

A spectrophotometric method utilizing the dye indigo carmine has been applied to the analysis of dissolved oxygen in water samples. Oxygen concentration has been determined by the decrease in absorbance at 410 mμ of reduced indigo carmine solutions oxidized by dissolved oxygen. A simple modification of the sample compartment of a Bausch and Lomb Spectronic 20 or 340 spectrophotometer allows rapid and accurate measurements to be made within 3 min. Dissolved oxygen in the ranges of 0 to 10% and 0 to 100% saturation can be analyzed without many of the interferences inherent in the standard Winkler method.     

Determination of dissolved oxygen in water

Dissolved oxygen in water is determined by its oxidation of manganese(II) to manganese(III) in alkaline medium and formation of the red manganese(III) ethylenediaminetetra-acetic acid complex on acidification to pH 4. The range of determination is 7-3160 mug of oxygen in a final volume of 500 ml.     

A neutron activation procedure for the determination of dissolved silver in sea water

A neutron activation procedure has been developed for the determination of silver in sea water. The element is preconcentrated by an anion-exchange procedure. The concentrate is submitted to irradiation with thermal neutrons. Silver-11Om is separated from other radionuclides by means of a conventional radiochemical separation scheme. The method gave a coefficient of variation of ± 10% at a silver level of 40 ng l^?1.     

Use of radioactive kryptonate of thallium in the determination of oxygen dissolved in water or other liquids

Radioactive kryptonate of thallium is placed in the liquid sample. Oxygen dissolved in the sample reacts with the surface layer of radioactive kryptonate of thallium, and releases radioactive krypton in amount proportional to the amount of oxygen.     

A new method for the determination of oxygen in organic compounds

Oxygen in compounds of carbon, hydrogen, and oxygen can be determined by heating the sample with an excess of strontium oxide and graphite in. a nickel bomb or sealed Vycor glass tube. During the heating period, three hours at 650° C, the oxygen of the sample is converted to carbonate. The carbonate is then determined volumetrically. The accuracy of the method was found to be ± 0.3% (absolute percentage error) for several types of compounds. Most elements other than carbon, hydrogen, and oxygen interfere. Compounds like phenol, that are exceedingly resistant to complete pyrolysis, yield low resuilts. Carbon in organic compounds can be determined by heating the sample with barium nitrate, and subsequently determining carbonate in the mixture.     

A manometric method for the determination of oxygen in organic compounds

Summary A vacuum apparatus is described for the determination of oxygen in 3 to 5 mg of organic substance. The oxygen of the substance is converted to carbon monoxide by ignition in a bomb at 1050 to 1055° C. Corrections are calculated from thermodynamic data for the amounts of water and carbon dioxide not reacting at the ignition temperature.

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Zusammenfassung Eine Vakuumapparatur für die Bestimmung des Sauerstoffes in 3 bis 5 mg organischer Substanz wird beschrieben. Der in der Substanz enthaltene Sauerstoff wird durch Erhitzen auf 1050 bis 1055° C in einem geschlossenem Quarzrohr in Kohlenmonoxid übergeführt, das dann in der Vakuumapparatur zu Kohlendioxid oxydiert und durch Absorption gemessen wird. Korrekturen werden aus thermodynamischen Daten für die bei der Verbrennungstemperatur nicht reagierenden Wasser- und Kohlendioxidmengen berechnet.

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Résumé On décrit un appareil á vide pour le dosage de l'oxygéne sur 3 á 5 mg de substance organique. On convertit l'oxygéne de la substance en oxyde de carbone par combustion dans une bombe, á 1050–1055° C. On calcule les corrections á partir des données thermodynamiques pour l'eau et le gaz carbonique qui ne réagissent pas á cette température.

     

Micro-Winkler titration method for dissolved oxygen concentration measurement

In this report a gravimetric micro-Winkler titration method for determination of dissolved oxygen concentration in water is presented. Mathematical model of the method taking into account all influence factors is derived and an uncertainty analysis is carried out to determine the uncertainty contributions of all influence factors. The method is highly accurate: the relative expanded uncertainties (k = 2) are around 1% in the case of small (9-10 g) water samples. The uncertainty analysis carried out in characterizing the uncertainty of the method is the most comprehensive published for a micro-Winkler method, resulting in experimentally obtained estimates for all uncertainty sources of practical significance (around 20 uncertainty sources altogether).     

A novel sensor based on the porous plastic probe for determination of dissolved oxygen in seawater

A new sensor based on the porous plastic probe has been developed for the detection of dissolved oxygen. This probe was prepared by co-polymerization of monomer, cross-linking reagent, porogent and luminescent ruthenium(II)diimine complex. The porous plastic probe exhibits good response to dissolved oxygen and resistance to indicator leaching out due to its high hydrophobicity. The preparation and characteristics of the probe were investigated in detail. This porous plastic probe serves as analyte-sensitive function as well as optical wave-guide, which make it easy to assemble the fiber-optical chemical sensor (FOCS). The developed sensor has been applied to the determination of dissolved oxygen in seawater with satisfactory results compared with the standard method.     

A rapid method for the determination of radiostrontium in river water

A rapid analytical method, applicable for the selective separation and determination of⁹⁰Sr and⁸⁹Sr in river water, is described. Strontium is extracted from the water sample at pH 10.5 by TTA/TOPO in cyclohexane in the presence of Tiron as masking agent for interfering ß-emitters. Radiostrontium is measured by liquid scintillation after back-extraction into 1N nitric acid. The distribution coefficient of strontium is over 400 and the separation factors from other radionuclides are higher than 5.0×10³.     

A novel method for the spectrophotometric determination of nitrite in water

A rapid, simple, selective and sensitive method for the spectrophotometric determination of nitrite in water has been developed and optimum reaction conditions along with other analytical parameters have been evaluated. Nitrite reacts with barbituric acid in acidic solution to give the nitroso derivative, violuric acid. At analytical wavelength of 310 nm, Beer's law is obeyed over the concentration range 0.00–3.22 ppm of nitrite. The molar absorptivity is 15330 ± 259.7 (95%) with pooled standard deviation of 355.57 and R.S.D. of 2.32%. As well as the method is sensitive (2.99 × 10⁻³ μg NO₂ cm⁻²) and selective, it tolerates most of the potential interferents. It has been successfully applied to nitrite determination in natural waters by use of a calibration graph with determination limit of 1.66 μg NO₂ in 100 mL working solution corresponding to minimum 9.5 ppb NO₂–N in water samples. Lower concentrations of nitrite (3.0 μg NO₂/L sample) is precisely analyzed by using the method of dilution with sample, with R.S.D. of lower than 0.5%. The results were compared with standard N-(1-naphtyl)ethylenediamine dihydrochloride method and very good agreement between the data was observed. The method can easily be applied in the field.     

A voltammetric method for diuron determination in river water

A sensitive, simple, fast, and inexpensive method for determining diuron in water using square wave voltammetry and a glassy carbon electrode is presented. This method was developed to evaluate diuron contamination in river waters close to sugarcane cultivation, located in the metropolitan region of João Pessoa, in the state of Paraíba, Brazil. An analytical curve with a linear response ranging from 38.5–115.0 nmol L⁻¹ (r² = 0.993), a LOD equal 0.2 nmol L⁻¹, and recovery rates from 88.0 to 108.0 %. The proposed method does not require any previous chemical treatment of the sample, thus contributing to green analytical chemistry.