Ice pillar, which means ice stalagmite linked to icicle in this paper, was formed in the cold room and the height of it was 185 cm. The growth processes of the ice pillar were estimated from the ice structures in the horizontal and vertical cross sections. The whole ice pillar consists of many ice crystals. Judging from the discontinuity of the ice structure, it can be presumed that the lower part of the ice pillar which had grown upward were linked to the upper part which had grown downward at around 170cm high. Either parts has different ice structure from the natural ice stalagmite or icicle, because too much water dropped intermittently and the air temperature in the cold room was too low during the ice pillar grew
A study was made of the petrology of a variety of underground ice types in permafrost on the Tuktoya...
Abstract. We have investigated the formation of 10-50 mm long “ice spikes ” that sometimes appear on...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...
International audienceFor the first time, to our knowledge, a scientific study of the formation and ...
The formations of the ice spike, which is the ice bar risen upward from the ice surface in bowl and ...
This paper will give a historical overview of ice structures with a focus on the construction method...
For the sake of studying the morphology and the growth mode of single snow crystals forming in the p...
The growth mechanisms of long prisms with skeletal structures precipitating in the polar regions are...
The Hokkaido University Alaskan Glacier Expeditions carried out field studies on the mecha-nisms of ...
The morphological instability and the growth mechanism of ice crystals grown in air at -30℃ and at s...
Ice crystals were produced in a supercooled cloud by seeding rock-forming minerals and clay minerals...
In-situ observations of needle ice crystals growing in air at 10^5 Pa at -7℃ and at about water satu...
In order to study the morphology and the growth mechanisms of single snow crystals observed in polar...
Ice crystallographic measurements have been made on eight cores retrieved from temperate Glacier de ...
A study was made of the petrology of a variety of underground ice types in permafrost on the Tuktoya...
Abstract. We have investigated the formation of 10-50 mm long “ice spikes ” that sometimes appear on...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...
International audienceFor the first time, to our knowledge, a scientific study of the formation and ...
The formations of the ice spike, which is the ice bar risen upward from the ice surface in bowl and ...
This paper will give a historical overview of ice structures with a focus on the construction method...
For the sake of studying the morphology and the growth mode of single snow crystals forming in the p...
The growth mechanisms of long prisms with skeletal structures precipitating in the polar regions are...
The Hokkaido University Alaskan Glacier Expeditions carried out field studies on the mecha-nisms of ...
The morphological instability and the growth mechanism of ice crystals grown in air at -30℃ and at s...
Ice crystals were produced in a supercooled cloud by seeding rock-forming minerals and clay minerals...
In-situ observations of needle ice crystals growing in air at 10^5 Pa at -7℃ and at about water satu...
In order to study the morphology and the growth mechanisms of single snow crystals observed in polar...
Ice crystallographic measurements have been made on eight cores retrieved from temperate Glacier de ...
A study was made of the petrology of a variety of underground ice types in permafrost on the Tuktoya...
Abstract. We have investigated the formation of 10-50 mm long “ice spikes ” that sometimes appear on...
Ice crystals were grown in free fall by using a large cloud chamber of height 6.5m. Nucleation was c...