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E20 fiveeasy ph meter

Manufactured by Mettler Toledo
Sourced in Germany

The E20-FiveEasy pH meter is a laboratory instrument designed to measure the pH value of liquid samples. It features a large, backlit LCD display and simple, intuitive operation. The device is suitable for a variety of applications requiring accurate pH measurement.

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2 protocols using e20 fiveeasy ph meter

1

Soil and Climate Influence on Ecosystem

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The environmental parameters were geographic variables (latitude, longitude, and elevation) and meteorological data [mean annual precipitation (MAP) and mean annual temperature (MAT)] at each sampling site and soil properties [pH, electrical conductivity (EC), total carbon (TC), total nitrogen (TN), and the TC/TN ratio] for each sample. The meteorological data (MAP and MAT) were collected from the Chinese Meteorological Agency Database1. Soil pH was measured by using an E20-FiveEasy pH meter (Mettler Toledo, Giessen, Germany), and the soil EC was calculated by using an electric conductometer. Both soil measurements used a soil water suspension (a 5:1 vol/vol mixture of deionized water and soil) after shaking for 30 min. Soil TC and TN were determined with a carbon–hydrogen–nitrogen elemental analyzer (2400 II CHN Elemental Analyzer; PerkinElmer, Boston, MA, United States). Meteorological data and soil properties are shown in Supplementary Tables 1, 2, respectively.
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2

Soil Physicochemical Properties Assessment

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Soil pH was measured by using an E20-FiveEasy pH meter (Mettler Toledo, Germany), and soil electrical conductivity, the indicator of soil soluble salt, was determined by using an electric conductometer. Both soil measurements were made using a soil-water suspension (5:1 mixture of deionized water-fresh soil) after shaking for 30 min. Soil moisture was determined gravimetrically at ∼105°C for 6 h. Dissolved total nitrogen (DTN), nitrate (NO3-N), and ammonium (NH4+-N) were extracted by adding 5 g fresh soil to 50 ml of a 2 M KCl solution, and dissolved organic carbon (DOC) was extracted with 50 ml of deionized water. After shaking for 1 h and standing for 1 h, the supernatant was filtered through glass fiber filters (Fisher G4, 1.2-μm pore space). The concentrations of NO3-N, NH4+-N, and DTN were determined using a continuous-flow analytical system (San++ system; Skalar, Holland). DOC was determined by using a carbon nitrogen analyzer (Multi N/C 3000; Analytik Jena, Germany). Available phosphorus (P) was extracted with a 0.5 M NaHCO3 solution and measured by the Mo-Sb colorimetric method. Available potassium (K) was extracted with 1 M ammonium acetate (NH4OAc) and measured by the flame spectrophotometry method. Soil organic matter (SOM) was measured by the K2Cr2O7-H2SO4 oxidation method, and total nitrogen (TN) was measured by the Kjeldahl method.
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