J T Volk Fermilab April 2008 Ground Motion Studies at Fermi National Accelerator Laboratory James T Volk Applications Physicist II Vladimir Shiltsev, Shavkat.

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Presentation transcript:

J T Volk Fermilab April 2008 Ground Motion Studies at Fermi National Accelerator Laboratory James T Volk Applications Physicist II Vladimir Shiltsev, Shavkat Singatulin

J T Volk Fermilab April 2008 Fermilab 40 miles due west of Chicago Illinois World’s highest energy particle accelerator Site is 6800 acres, 10 sections, 2752 hectares The Tevatron 1 km radius tunnel 30 feet below surface Protons and anti protons collide at center of mass energy of 1.9 Tev Beam size is 0.1 mm Cultural noise is an issue

J T Volk Fermilab April 2008 Fermilab World’s highest energy particle accelerator Site is 6800 acres 10 sections 2752 hectares The Tevatron 1 km radius tunnel 30 feet below surface Protons and anti protons collide at center of mass energy of 1.9 Tev Beam size is mm Cultural noise is an issue Tevatron 1 km radius

J T Volk Fermilab April 2008 Fermilab World’s highest energy particle accelerator Site is 6800 acres 10 sections The Tevatron 1 km radius tunnel 30 feet below surface Protons and anti protons collide at center of mass energy of 1.9 Tev Beam size is mm in diameter Cultural noise is an issue EJ&E rail road

J T Volk Fermilab April 2008 Future projects at Fermilab Project X is an 8 GeV Linear Accelerator To replace old LINAC And booster Muon Collider is a High intensity muon and Neutrino facility

J T Volk Fermilab April 2008 International Linear Collider Two linear accelerators each 15 miles long colliding electrons and anti electrons. Beam size nanometers (10 -9 meters). Cultural and natural sources of noise will cause problems such as beam dispersion and lower luminosity (particles /cm 2 sec). Two tunnels are proposed one for the accelerator and the other for power supplies. The US proposed site is at Fermilab in Illinois.

J T Volk Fermilab April 2008 Ground motion at Fermilab All these accelerators and Detectors are sensitive to Cultural noise traffic, HVAC, water, and, vacuum pumps. Natural noise tides, earth quakes motion due to ground water

J T Volk Fermilab April 2008 Simple HLS system h1 h2

J T Volk Fermilab April 2008 Simple HLS system h1 h2

J T Volk Fermilab April 2008 Plumbing There are two types of systems Fully filled or two pipe systems –Two pipes one for water one for air –The water pipe can change in elevation i.e. snake around obstacles –Temperature variations can effect data Half filled or one pipe system –One pipe must be level –Problems with air bubbles and water blocks –Less dependence on temperature and pressure variation

J T Volk Fermilab April 2008 Hydro static water Level Systems HLS BUDKER sensor Accuracy 1 micrometer Cost $1200 per channel Ultra sonic sensor better than 1 micrometer $3500 per channel Capacitive sensor Water pool On stand with water and Air line connections

J T Volk Fermilab April 2008 Fermilab HLS sensors Balluff proximity sensor Air line Water line Accuracy 6 micrometers Cost $120 - $140 per channel

J T Volk Fermilab April 2008 HLS systems at Fermilab Fermilab system installed on all quads in Tevatron 204 sensors covers 6 kilometers 4 BUDKER sensors in MINOS hall 100 meters below grade on top of Galena Platteville dolomite. We have added 3 more sensors at 90 degrees with respect to original line. 5 sensors in LaFarge mine in North Aurora Illinois 120 meters below ground in Galena Platteville dolomite (down at present time moving to new drift) 11 Fermilab sensor in NMS hall 7 sensors on the low beta quads at both B0 and D0 collision halls 40 sensors on Tevatron quads in B sector (no longer operational) 40 sensors in MI-8 beam line (no longer operational)

J T Volk Fermilab April 2008 MINOS System Long base line Neutrino experiment At Fermilab with Neutrinos are also Detected at Soudan Mine in Minnesota 100 meters below Grade on top of Galena Platteville Dolomite 4 sensors 30 meters Apart along western wall

J T Volk Fermilab April 2008 Layout of MINOS water level MINOS detector 30 meters Not to scale  direction Sensor Water line Depth of floor 100 meters below grade 406 feet above sea level Maquoketa shale Location of Horizontal and Vertical seismometer New sensors

J T Volk Fermilab April 2008 MINOS Tidal Data Difference in two sensors 90 meters apart Pressure Kpsa difference

J T Volk Fermilab April 2008 January 2006 MINOS Difference in two sensors 90 meters apart temperature

J T Volk Fermilab April 2008 January 2006 MINOS Difference in two sensors 90 meters apart

J T Volk Fermilab April 2008 Sump Pump test

J T Volk Fermilab April 2008 Difference in two sensors 90 meters apart MINOS hall 27 months of data

J T Volk Fermilab April 2008 Subsidence and Tremors

J T Volk Fermilab April 2008 LaFarge Mine North Aurora There is a dolomite mine 7 km from the MINOS hall. It is in the Galena Platteville layer 125 meters below the surface. It is room and pillar Construction There are 5 HLS sensors in an abandoned drift in the mine.

J T Volk Fermilab April 2008 Difference in two sensors 60 meter apart

J T Volk Fermilab April 2008 Difference in two sensors150 meters apart 18 months of data

J T Volk Fermilab April 2008 Summary There are several HLS system taking data at Fermilab The data are available at y/index y/index There are natural sources of motion tides for example There are cultural sources such as sump pumps Plans for new systems in the works