Capability Improvements of the NMISA Humidity Laboratory

Slides:



Advertisements
Similar presentations
GY205 Weather and Climate Lecture 3.
Advertisements

HUMIDITY AND DEW POINT.
MOLLIER DIAGRAM.
Section 04 Thermodynamics Adiabatic Processes Lesson 10/11.
After completing this Lesson, you will be able to answer: 1. What is humidity? 2. What is relative humidity? 3. How relative humidity is measured? 4. What.
Elevation It gets colder the higher in elevation you go. As air rises, it expands because of lower air pressure. As the air expands, it cools. When air.
Humidity First let us consider five humidity variables
Understanding Weather Water in the Air Ch. 2 Sec. 1 p
Lecture Saturation The level you’ve reached by week 4 of the semester.
HUMIDITY. ABSOLUTE HUMIDITY: Absolute humidity (expressed as grams of water vapor per cubic meter volume of air) is a measure of the actual amount of.
Humidity. Water Vapor Can make up as little as 1/10 th of 1% to 4% of the atmosphere. Scientists agree that it is the most important atmospheric gas when.
Miruna DOBRE – SMD (Belgium) Stephanie BELL – NPL (United Kingdom) Dolores del CAMPO – CEM (Spain) Martti HEINONEN - MIKES (Finland)
© NMISA 2010 INTERNATIONAL ACTIVITIES AT THE NMISA HUMIDITY LABORATORY DURING 2009/2010 Deona Jonker.
A FIRST REVIEW OF CALIBRATION DEVICES ACCEPTABLE FOR METROLOGY LABORATORY Mr Drago GROSELJ Dr Jérôme DUVERNOY Dr John GORMAN
Moisture Variables on Skew T Log P Diagram AOS 330 LAB 8.
Saturation = filled to capacity
How much moisture is in the air relative to how much it can hold
HUMIDITY AND DEW POINT. CONDENSATION � H2O can exist in solid, liquid, or gaseous states. Change from liquid to gas is evaporation. Change from gas to.
EG1204: Earth Systems: an introduction Meteorology and Climate Lecture 3 Evaporation and humidity.
Concept of Humidity What is the relationship between water vapor holding and temperature? Air hold more water vapour at higher temperature.
By: Group 1 By: Group 1. At daytime, sunlight warms the Earth. Through conduction, air near the ground warms up.conduction conduction between the air.
Bell work Observe two glasses of water. One is filled with ice water, and one is filled with warm water. Why do water droplets form on the outside of the.
Parameter's Approach to Relative Humidity Control August 25, 2011 by Clay Hile.
HUMIDITY AND AIR CONDITIONING
Humidity Water Vapour in the Air. The more water vapour in the atmosphere A) the air becomes heavier. B) the air becomes lighter. C) the air stays the.
 Both chilled mirror devices lag the fast Ly-α TWC by an amount dependent on mixing ratio and phase of water on mirror. Facility for Airborne Atmospheric.
I. Water’s Changes of State 18.1 Water in the Atmosphere  A) Precipitation is any form of water that falls from a cloud.  1) When studying the ATM, H20.
Chapter 18 Moisture, Clouds, and Precipitation When it comes to understanding atmospheric processes, water vapor is the most important gas in the atmosphere!
© NMISA 2010 THE 2009/2010 SANAS COMPARISON FOR HUMIDITY Deona Jonker.
Atmospheric Moisture (Text Pg 84-92)
Behaviour of agricultural/food materials under stress
HUMIDITY AND DEW POINT.
Atmospheric Sciences 101 Humidity.
Unit 4 Weather ©Mark Place,
Humidity The absolute humidity is the mass of the water vapor in a given volume of air or gas. It’s unit of measurement is grams per cubic meter.
Bell work Observe two glasses of water. One is filled with ice water, and one is filled with warm water. Why do water droplets form on the outside of the.
Humidity.
Introduction to Climate
Do Now & Announcements Turn in shaving cream lab if you did not do so last class Get Heat HW stamped Answer Heating Curve Questions Today: Solubility.
Water in the Atmosphere
Moisture and Clouds Current Weather Humidity Clouds
Water’s Changes of State
Water’s Changes of State
2.5.4c Moisture, Precipitation, and Clouds
AIM: DO NOW: HW:.
Weather and Climate – Part 2
Clouds and Cloud Formation
Readout units and the calibration of loadcells.
Unit 4 Weather about Doppler Radar.
Weather Part I Revised 2010 Revised 2010 ©Mark Place,
Atmospheric Sciences 101 Humidity.
Water in the Atmosphere
Clouds and Cloud Formation
Weather ©Mark Place,
Day 9 - Humidity Science 10 Weather.
About 71% of the Surface of the Earth Is Covered with Water.
Near Ambient Temperature Control & Humidity Control
Atmospheric Sciences 101 Humidity.
FIGURE 4.4 The water vapor content (humidity) inside this air parcel can be expressed in a number of ways. Fig. 4-4, p.80.
What do scientists measure?
Weather and Humidity 1.
11.2 State of the Atmosphere
Chem Get Heat HW stamped Answer Heating Curve Questions
Water in the Atmosphere
Due tomorrow before class starts: Definition of all vocab words in Chapter 11, Section 2 Temperature Versus Heat Skip about 4-5 lines in-between each.
Water in the Atmosphere
Moisture in the Atmosphere
Presented By: T.M Ramashidzha Metrology Scientist
Atmospheric Moisture and Stability
Presentation transcript:

Capability Improvements of the NMISA Humidity Laboratory Capability Improvements of the NMISA Humidity Laboratory Regina Mnguni, NMISA 31 July 2017 TQM-5134-1

Outline Introduction What is humidity? Current capabilities Improvements Conclusion TQM-5134-1

Introduction NMISA Humidity laboratory maintains the national humidity standards and disseminate the traceability to industry. The laboratory has been SANAS accredited since the year 2004. The lab’s capabilities cover the low dewpoint temperature range and relative humidity parameters only. TQM-5134-1

Introduction continue… The humidity lab wants to increase/improve the capabilities: To include high dewpoint temperature range Establish traceability of relative humidity to temperature, pressure and dewpoint temperature To include water activity parameter TQM-5134-1

What is Humidity? Humidity is the amount of water vapour present in air or other gases. Humidity terms/parameters Relative humidity - the ratio of actual vapour pressure to the saturation vapour pressure at the same temperature, expressed as a percentage (%) Dewpoint Temperature – the temperature at which dew/frost or condensation forms on a cooling gas. The temperature at which air becomes saturated in equilibrium with water. TQM-5134-1

What is Humidity? continue Water activity – the ratio of the vapour pressure of water in a material to the vapour pressure of pure water at the same temperature. It is the same as equilibrium relative humidity (ERH) except that it is expressed on a scale of 0 to 1. TQM-5134-1

Current capabilities Relative humidity 5 %rh to 95 %rh range covered at 5 °C to 55 °C. Unsaturated salts are used at the temperature range 15 °C to 30 °C. Thermohygrometer is used at 5 °C to 55 °C in a controlled chamber. TQM-5134-1

Current capabilities continue Dewpoint temperature The range covered is from -75 °C to +17 °C A pressure swing dryer, flow mixing generator and two chilled mirror hygrometers used as a system. Hygrometer Hygrometer Flow mixing generator Pressure swing dryer TQM-5134-1

Improvements Water activity measurements Calibration of the meters using unsaturated salts. In the process of acquiring accreditation TQM-5134-1

Improvements continue… Two pressure humidity generator/chamber procured together with a dewpoint meter. To replace the old climatic chamber of 20 years Old controlled chamber Two pressure generator/chamber TQM-5134-1

Improvements continue… To be used for the calibration of relative humidity instruments (i.e. data loggers, weather stations, indoor air quality monitors and thermohygrometers). To extend the dewpoint temperature range to +70 °C. The temperature range of the chamber is -10 °C to +70 °C. The principle of operation (2 pressure) is that the gas is humidified at elevated pressure then expanded to a lower pressure at the given temperature. TQM-5134-1

Improvements continue… The chamber will be used concurrently with the calibrated dewpoint meter to give traceability for relative humidity calibrations. This will replace the traceability to salt solutions and make NMISA comparable with other NMIs in RH. TQM-5134-1

Conclusion With the new method/equipment, UoM for relative humidity will be improved. NMISA humidity lab to offer calibration of dewpoint meters of a higher range. NMISA humidity lab will offer traceability for the water activity meters. TQM-5134-1

TQM-5134-1