Abstract
Groundwater storage in an atoll island facing water shortage is a crucial issue for freshwater supply and agriculture. A floating-type underground dam is proposed as a solution for shortage of freshwater in an atoll island. Precipitation infiltrates into, displaces brine in underground and is stored as freshwater resources. In south part of Japan, the aquifer in an atoll of them consists of vuggy limestone, “Ryukyu-limestone”, with a wide range of pore sizes and heterogeneous pore structure so that retardation in salinity reduction from pore water in aquifer controls freshwater reservation. To understand the pore structure in the vuggy limestone, X-ray CT scannings were carried out for eighteen cores of Ryukyu-limestone with different size, 100, 50 and 6 mm in diameter. Cluster analysis for three-dimensional distribution of pore demonstrates that Quaternary vuggy Ryukyu-limestone has a binary fractal in a wide range of size distribution with 13 orders (from 1.0×10−17 m3 to 1.0×10−5 m3) for pore volume and with 11 orders (1.0×10−11 m2 to 1.0×10−1 m2) for pore surface area. Our numerical approach suggests that three-dimensional pore structure of Ryukyu-limestone aquifer can be modelled by binary fractal aggregation of spheres of various size.
Groundwater storage in an atoll island facing water shortage is a crucial issue for freshwater supply and agriculture. As a solution to increase the volume of freshwater in an atoll, a floating-type underground dam is proposed (Okinawa General Bureau and Ministry of Agriculture, Forestry and Fisheries, 2008). Precipitation infiltrates into, displaces brine in underground and is stored as freshwater resources.
The aquifer in an atoll of them consists of vuggy limestone, “Ryukyu-limestone”, with a wide range of pore sizes and heterogeneous pore structure. It is concerned that brine in dead-end pore can cause retardation in salinity reduction in aquifer for freshwater reservoir (Masuoka, 2016). So that in order to predict behavior of freshwater in a floating-type underground dam, it is important to reveal pore structure of the vuggy limestone and the mechanism how the retardation in salinity reduction proceeds in the rock pore structure.