Santiago Martín González

Learn More
Globally, the methane (CH4) efflux from the ocean to the atmosphere is small, despite high rates of CH4 production in continental shelf and slope environments. This low efflux results from the biological removal of CH4 through anaerobic oxidation with sulfate in marine sediments. In some settings, however, pore water CH4 is found throughout the(More)
__We investigate the application to biomimetics on the development and creation of a new type of exterior walls for buildings. We study and explore envelopes as found in nature with an eye on their application to architecture and engineering. Our hypothesis is the following: Is it possible to obtain greater efficiency and performance in the construction of(More)
  • 1