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Hi 2550

Manufactured by Hanna Instruments
Sourced in Italy

The HI 2550 is a benchtop pH/mV/°C meter from Hanna Instruments. It features a large LCD display and user-friendly interface. The device can measure pH, mV, and temperature parameters.

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6 protocols using hi 2550

1

Peat Soil Chemical Analysis Protocol

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Peat samples were homogenized and topped with distilled water in a 10:1 (H2O: sample) v/w ratio. Samples were mixed with water and endured for 12 h. The suspension was filtered, and the filtrate was used for further chemical analysis. рН was measured by pH-meter HI 2550 (HANNA instruments, Italy). Concentrations of mineral nitrogen (NH4+, NO2+, NO3+) and soluble phosphates in the filtrate were measured by spectrophotometer Hach Lange DR3900 (Hach, USA) in 1 inch square glass cuvettes according to the standard manufacturers’ instructions that correspond to the following methods of water analysis certified by EPA Environmental Protection Agency (USA) (Rice and Bridgewater, 2012 ). In brief, the concentration of NO2 was measured by the diazotization method (reagent set NitriVer 3, Hach), the concentration of NO3− was measured by the cadmium reduction method (reagent set NitraVer 6, Hach), the salicylate method was used to measure NH4+ (Nitrogen-Ammonia Reagent Set, Hach), and ascorbic acid method was used to measure concentration of PO43− (reagent set PhosVer 3). Nitrate Standard Solution (100 mg/L), Nitrite Standard Solution (250 mg/L NO2-N), Ammonium Standard Solution (50 mg/L), Phosphate Standard Solution (50 mg/L as PO43−, NIST) provided by Hach (USA) were used to build the calibration curves. All measurements were performed in triplicates at 18°C.
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2

Determining Free Acidity and pH in Honey

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Free acidity and pH measurement was done by AOAC (1990) method number 962.19 using a pH meter (HANNA, HI 2550, PH/ORP). Free acid (meq of acid/1000 g) was determined by dissolving a honey sample (10 g/75 mL distilled water) and titrating with standardised 0.1 M NaOH to pH 8.3 using a pH glass electrode attached to pH meter (Consort C861, Belgium) as end point indicator.
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3

Electrical Conductivity Measurement of Honey

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A conductivity meter (HANNA, HI 2550, EC/TDS/NaCl meter) was used to determine electrical conductivity. The honey solution (20% w/v) was suspended in deionized water (Bogdanov, 2009 ). The electrical conductance of this solution was read in mS after the temperature has been equilibrated to 20 °C (AOAC 1990 ). Anhydrous honey (20 g) was dissolved in distilled water. The solution was transferred quantitatively to a 100ml volumetric flask and made up to volume with distilled water. After the temperature had been equilibrated to 20 °C, the electrical conductance of this solution was measured in milliseconds. The honey solution's electrical conductivity was measured using the formula below (Equation 3). SH=K×G Where SH = electrical conductivity of the honey solution in mS.cm−1, K = cell constant in cm−1, G = conductance in mS.
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4

Plasma-Treated Solution Analysis

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The acidity and redox potential of plasma-treated solutions were measured using a pH electrode (HI1131) and a redox electrode (HI3148B) connected to the device “HANNA instruments HI2550”. All measurements were carried out immediately after treatment of the solutions with cold plasma and an hour later. The concentrations of hydrogen peroxide, nitrite, hypochlorite, pH, and redox potential did not change within an hour after treatment.
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5

Measuring pH of Food Blends

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The pH meter (Hi 2550, Hanna Instruments) was used to determine the pH of the formulated cassava-cowpea-orange-fleshed sweet potato (OFSP) blends in triplicates. 1 g of flour was reconstituted in 10 ml of distilled water and shaken vigorously [25 ].
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6

Soil Properties and Landscape Factors

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The co-variates are subdivided in the following categories: climate, soil, land use and biological indicators. Soil pH was measured in a suspension (1:2 w:w) of 1 M KCl using a pH meter (HI2550 Hanna Instruments). Apart from the pH, the climate and soil related co-variates were derived at the 89 sites from thematic maps (Table 2). The upstream flow length and crop cover (C) factor were used as in the RUSLE equation (Renard et al., 1991) .
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