Montana State University's Subzero Science and Engineering Research Facility: New Interdisciplinary Cold Regions Research Laboratories

Montana State University recently completed construction and commissioning of a low temperature research facility with funding from the National Science Foundation, Murdock Charitable Trust and Montana State University. The Subzero Science and Engineering Research Facility (housed in the Department of Civil Engineering) supports a broad range of cold regions research disciplines including structural, soil, asphalt, concrete, geosynthetics, life sciences, ice/snow mechanics, wetlands, streams, transportation, and earth sciences. The simulated environments are applicable from medium/low latitude winter to polar. The facility has several world unique capabilities in environmental simulation and includes eight walk in cold laboratories, three smaller low temperature biological incubators/ environmental chambers, a low temperature epifluorescence microscope, and a temperature controlled computed tomography (CT) scanner. Each of the laboratories, while adaptable for broad application, is designed with a specific scientific focus in mind. Functions of the fully programmable individual cold laboratories include: units that provide simulation of solar and sky radiation providing realistic energy balance, a large scale structural engineering test bed, a class 1000 clean room with class 100 work area, a unit in which the liquid water phase maintains an influential environmental role, room for specimen storage, a teaching laboratory with ample room for student groups and general specimen preparation area. The paper summarizes the specific capabilities of each chamber and describes the ongoing and future research in these facilities.

[1]  T. Palys,et al.  Evaluation of disinfectant efficacy against biofilm and suspended bacteria in a laboratory swimming pool model. , 2004, Water research.

[2]  H. Rifai,et al.  Review of MTBE Biodegradation and Bioremediation , 2003 .

[3]  Howard Conway,et al.  Snow stability during rain , 1993, Journal of Glaciology.

[4]  E. Adams,et al.  Model for effective thermal conductivity of a dry snow cover composed of uniform ice spheres , 1993, Annals of Glaciology.

[5]  H. Conway,et al.  Infiltration of water into snow , 1994 .

[6]  E. Adams,et al.  Evaluation of snow-surface energy balance models in alpine terrain , 2003 .

[7]  J. Priscu,et al.  Impact of Episodic Warming Events , 2004 .

[8]  O. Stein,et al.  Does batch operation enhance oxidation in subsurface constructed wetlands? , 2003, Water science and technology : a journal of the International Association on Water Pollution Research.

[9]  A. Camper Involvement of humic substances in regrowth. , 2004, International journal of food microbiology.

[10]  R. H. McBee INTESTINAL FLORA OF SOME ANTARCTIC BIRDS AND MAMMALS , 1960, Journal of bacteriology.

[11]  Michael Lehning,et al.  A statistical validation of the snowpack model in a Montana climate , 2001 .

[12]  S. Colbeck,et al.  An overview of seasonal snow metamorphism , 1982 .

[13]  P. Stewart,et al.  Hypothesis for the Role of Nutrient Starvation in Biofilm Detachment , 2004, Applied and Environmental Microbiology.

[14]  O. Stein,et al.  Ammonium Removal in Constructed Wetland Microcosms as Influenced by Season and Organic Carbon Load , 2005, Journal of environmental science and health. Part A, Toxic/hazardous substances & environmental engineering.

[15]  O. Stein,et al.  Polar organic solvent removal in microcosm constructed wetlands. , 2005, Water research.

[16]  P. Stoodley,et al.  Detachment Characteristics and Oxacillin Resistance of Staphyloccocus aureus Biofilm Emboli in an In Vitro Catheter Infection Model , 2004, Journal of bacteriology.

[17]  J. Costerton,et al.  Pseudomonas aeruginosa Displays Multiple Phenotypes during Development as a Biofilm , 2002, Journal of bacteriology.

[18]  Birgit Sattler,et al.  Carbon Transformations in a Perennially Ice-Covered Antarctic Lake , 1999 .

[19]  A. Camper,et al.  Minimizing biofilm in the presence of iron oxides and humic substances. , 2002, Water research.

[20]  J. Heldmann,et al.  Polar Lakes, Streams, and Springs as Analogs for the Hydrological Cycle on Mars , 2005 .

[21]  R. Swanson,et al.  Snow Distribution Patterns in Clearings and Adjacent Forest , 1986 .

[22]  Philip S. Stewart,et al.  Modeling Antibiotic Tolerance in Biofilms by Accounting for Nutrient Limitation , 2004, Antimicrobial Agents and Chemotherapy.

[23]  J. Schimel,et al.  Interactions between Carbon and Nitrogen Mineralization and Soil Organic Matter Chemistry in Arctic Tundra Soils , 2002, Ecosystems.

[24]  P. Stewart,et al.  Pretreatment for membrane water treatment systems: a laboratory study. , 2003, Water research.

[25]  Anne K. Camper,et al.  Evaluation of Drinking Water Biostability Using Biofilm Methods , 2001 .

[26]  M. Schneebeli,et al.  Effect of snow structure on water flow and solute transport , 2004 .

[27]  J. Priscu,et al.  Distribution of organic carbon and nitrogen in surface soils in the McMurdo Dry Valleys, Antarctica , 2000, Polar Biology.

[28]  L. R. McKittrick,et al.  FORECASTING TERRAIN-DEPENDENT WEATHER CONDITIONS: DETAILS OF A MODEL CHAIN SEQUENCE , 2004 .

[29]  Anne K Camper,et al.  Chlorination of model drinking water biofilm: implications for growth and organic carbon removal. , 2002, Water research.