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This project aims to explore the causes of atmospheric electrical conductivity as altitude changes using a scientific balloon launch. The study will investigate correlations between air conductivity and cosmic ray activity, fluctuations due to meteorological events, and compare environmental factors' impact on conductivity. The technical setup involves measuring parameters like altitude, temperature, cosmic ray count, windspeed, and humidity. The study will provide valuable insights into cloud formations, thunderstorms, and other atmospheric phenomena.
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TEAM JUPITER KATHERINE BLACKBURN· SETH BURLEIGH · JOSEPH TRAN LaAces 2009-2010 Pre-Preliminary Design Review
MISSION GOAL Our goal is to investigate the causes of atmospheric electrical conductivity as a function of altitude. The launch will take place at the Columbia Scientific Balloon Facility (CSBF), in Palestine, Texas on May 25, 2010.
DEFINITIONS • Alpha Particles-ionizing forms of particle radiation • Aerosols-Small particles made up of atoms which • cling to nuclei in the atmosphere • Cosmic Ray-rays of highly energized particles from space • Humidity-Clouds, haze or other moisture collection in the atmosphere • Laminar Flow-flow of particles in a uniform direction • Shot Noise-Noise in the voltage measurement due to ions directly striking the inner electrode
SCIENCE GOALS • See if there exists any correlations between air conductivity and cosmic ray activity • Show uncharacteristic fluctuations in conductivity due to meteorological • events • Compare general profiles of temperature, pressure, humidity, and altitude with conductivity
SCIENCE BACKGROUND • WHAT IS ATMOSPHERIC ELECTRICAL CONDUCTIVITY? • The measure of • positive and • negative ions in • the atmosphere • Generally increases • with altitude Figure 1- Altitude as a function of conductivity. Most of the potential drop of the atmosphere occurs near the surface. Adapted from Reference 2.
SCIENCE BACKGROUND • WHAT AFFECTS ATMOSPHERIC ELECTRICAL CONDUCTIVITY? • Pollution level of air (e.g. aerosols) • Increased radiation in an area (e.g. cosmic • rays on the atmosphere) • Wind, pressure, moisture, and humidity • (i.e. factors that affect ion mobility) • IMPLICATIONS? • Cloud formations • Thunderstorms
SCIENCE BACKGROUND • PAST PROJECTS • Pollution measurements • based on surface • conductivity in • Mysore, India • Balloon payload in • Antarctica (Figure 2) Figure 2 – There is a quasi-sinusoidal behavior of the electrical field with respect to time as shown above. Adapted from Reference 2.
SCIENCE REQUIREMENTS • Must be able to sense small changes to see • uncharacteristic changes from surface to • 100,000 feet • Altitude and time must be measured • Cosmic ray intensity and atmospheric • conductivity data needs to be compared • for possible correlations
TECHNICAL GOALS • Measurement will occur from surface level to 100,000 feet • Target ascent rate is 1000 feet per minute • Altitude, temperature, cosmic ray count, windspeed, and humidity will need to be measured
TECHNICAL BACKGROUND THEORY OF OPERATION: VOLTAGE DECAY • Sample 1-2 Hz for 5-20 seconds • Reset Voltage
TECHNICAL BACKGROUND Equation 3 – Conductivity vs. exponential fit time constant Equation 4 – Capacitor current vs. combined Gerdien and measurement capacitance and change in outer-inner cylinder voltage Equation 5 – Conductivity Equation 6 – Theoretical cylindrical capacitor capacitance Equation - Gerdien capacitor current given V (outer voltage- inner voltage), L (length), a (conductivity), b(inner radius), and a (outer radius) Equation - Critical mobility - the minimum ion mobility (drift velocity/electric field) that will be captured by the gerdien capacitor
TECHNICAL BACKGROUND CRITICAL MOBILITY, ION CURRENT, BIAS VOLTAGE
TECHNICAL REQUIREMENTS • A voltage-sampling rate of 1 hertz (Hz) per 10 seconds (s) • Memory of 4050 bytes • At lower conductance (around 100 femtoSiemens) a 12 bit analog to digital converter with a 5 voltage (V) • The end of the inner electrode must be bullet shaped to promote laminar flow
REFERENCES (1/2) K. Nagaraja, B.S.N. Prasad, N. Srinivas, M.S. Madhava, Electrical conductivity near the Earth's surface: Ion-aerosol model, Journal of Atmospheric and Solar-Terrestrial Physics, Volume 68, Issue 7, April 2006, Pages 757-768, (http://www.sciencedirect.com/science/ article/ B6VHB-4JDMR5M-1/2/607a27d56c6adbf8ce265ea1ad0d8e0a) E.A. Bering, A.A. Few, J.R. Benbrook, The Global electric circuit, Journal of Physics Today, Volume 51, Issue 10, 1998, Pages 24-30 N. Ragini, T.S. Shashikumar, M.S. Chandrashekara, J. Sannappa, L. Paramesh, Temporal and vertical variations of atmospheric electrical conductivity related to radon and its progeny concentrations at Mysore, Indian Journal of Radio & Space Physics, Volume 37, August 2008, Pages 264-271 K.L. Aplin, A novel technique to determine atmospheric ion mobility spectra, Journal of Atmospheric and Oceanic Physics, January 2005, (arXiv:physics/0501129v1) K.L. Aplin, Instrumentation for atmospheric ion measurements, University of Reading Department of Meteorology, August 2000, Pages 1-274
REFERENCES (2/2) J.P. Scott and W.H. Evans, The electrical conductivity of clouds, Journal of Pure and Applied Geophysics, Volume 75, Issue 1, December 1969, Pages 219-232 (http://www.springerlink.com/content/x804k7123mqhn3r5/) R.G. Harrison, A.J. Bennett, Cosmic ray and air conductivity profiles retrieved from early twentieth century balloon soundings of the lower troposphere, Journal of Atmospheric and Solar-Terrestrial Physics, Volume 69, November 2006, Pages 515-527 K.A. Nicholl, R.G. Harrison, A double gerdien instrument for simultaneous bipolar air conductivity measurements on balloon platforms, Journal of Review of Scientific Instruments, Volume 79, August 2008 K.L. Aplin, R.G. Harrison, A computer-controlled gerdien atmospheric ion counter, Journal of Review of Scientific Instruments, Volume 71, Issue 8, August 2000 B. Balsey, (2009). Aerosol size distribution . Retrieved from http://cires.colorado.edu/science/groups/balsley/research/aerosol-distn.html