Abstract
The Japanese deep sea waters contain several recently discovered energy and mineral resources, such as methane hydrate and hydrothermal vents. This study examined the feasibility of in-situ ground improvement technologies for promoting precipitation of minerals based on in-situ microbial functions. The study also examined the solidification effect of deep-sea surface sediments. We sampled seawater from sea surface level to a depth of 750 m in the Toyama Bay using an oceanographic ship and carried out two types of calcium carbonate precipitation tests. The main findings of this research are as follows: (1) the population of urease-producing bacteria from sea surface to deep sea waters can enhance the 1-month cultivation and (2) these bacteria can accelerate the calcite precipitation.