Observations from the high resolution imaging science experiment (hirise) show dynamic landforms in the martian northern lowlands. One sign of activity, patterned ground, occurs nearly ubiquitously at…

Ended Grant For Research Awarded Last action

Contract number
80NSSC21K1093
Awardee
Awarding agency
Obligated
$291,968

Award facts

Contract value 100% obligated
$291,968.00 Current and potential, with all options
Completion date 100% complete
Current and potential, with all options
NAICS code
Not on record
Set-aside
No set-aside
Competition
Full and Open Competition Basic Research
Pricing
Other
Place of performance
College Station, TX, USA

Award details come from SAM.gov/FPDS.

Transactions

Action Obligated Date
Other Administrative Action P00003 · 20-MDAP20_2-0037, investigating boulder pattern formation and causes in the martian northern lowlands using spatial analysis of hirise images $0
Other Administrative Action P00002 · Investigating boulder pattern formation and causes in the martian northern lowlands using spatial analysis of hirise images $0
Funding Only Action P00001 $150,800
Original award $141,168

About this award

This federal contract award, with ID 80NSSC21K1093, was issued by the National Aeronautics and Space Administration (NASA) to Texas A&M University, a public research university in College Station, Texas. The $291,968 grant is for a two-year study to determine the origin of surface boulder distribution patterns in the Martian northern lowlands. The research will analyze high-resolution imaging data from the NASA HiRISE instrument to better understand periglacial processes on Mars, such as seasonal soil contraction and freeze-thaw cycles, and their impact on boulder movement and clustering. This work aims to fill a gap in the planetary science community's understanding of these Martian surface features. The contract does not have a set-aside designation, indicating Texas A&M competed for the award on an unrestricted basis.

Description

Observations from the high resolution imaging science experiment (hirise) show dynamic landforms in the martian northern lowlands. One sign of activity, patterned ground, occurs nearly ubiquitously at latitudes above ~60 n. IT is characterized by a polygonal network of fractures and forms from the seasonal contraction of the ICE-rich soil. Boulders clustered along the margins of the polygonal fracture networks may provide indirect evidence of polygon activity. Movement of boulders to the facture network margins could occur via diverse processes such as cyclical freezing-thawing, segregating ICE, or frost heaving, all of which are common processes in periglacial terrains on earth. Despite the ubiquity of the patterns and associated boulders, the spatial clustering of boulders, and their alignment to fracture margins, that could statistically show a relationship has not yet been quantified for much of the northern lowlands. That has deprived the planetary community of key parametric estimates in understanding the relationship of boulder clusters and polygonal terrain, and thus, represents a GAP in understanding of periglacial processes on mars. The overarching goal of this proposed two year study is to determine the origin of surface boulder distribution patterns in the martian northern lowlands.

Quick answers

Who was awarded contract 80NSSC21K1093?

80NSSC21K1093 was awarded to Texas A & M University by Shared Services Center (National Aeronautics and Space Administration) on August 20, 2021.

How much is contract 80NSSC21K1093 worth?

The government has obligated $291,968 on 80NSSC21K1093.

Was contract 80NSSC21K1093 competed?

The extent of competition for 80NSSC21K1093 was full and open competition.

On GovTribe

See this award's full record

  • Every transaction and funding action
  • The awardee's other awards and teaming partners
  • Similar awards and recompete opportunities
  • Ask GovTribe AI about this award