The Impact of Multiple Freeze–Thaw Cycles on the Microstructure of Aggregates from a Soddy-Podzolic Soil: A Microtomographic Analysis

Skvortsova, E.B.; Shein, E.V.; Abrosimov, K.N.; Romanenko, K.A.; Yudina, A.V.; Klyueva, V.V.; Khaidapova, D.D.; Rogov, V.V.

Авторы: Skvortsova E.B., Shein E.V., Abrosimov K.N., Romanenko K.A., Yudina A.V., Klyueva V.V., Khaidapova D.D., Rogov V.V.
Журнал: Eurasian Soil Science
Том: 51
Номер: 2
Год издания: 2018
Издательство: Maik Nauka/Interperiodica Publishing
Местоположение издательства: Russian Federation
Первая страница: 190
Последняя страница: 198
Оригинальные версии: ВЛИЯНИЕ МНОГОКРАТНОГО ЗАМОРАЖИВАНИЯ–ОТТАИВАНИЯ НА МИКРОСТРУКТУРУ АГРЕГАТОВ ДЕРНОВО-ПОДЗОЛИСТОЙ ПОЧВЫ (МИКРОТОМОГРАФИЧЕСКИЙ АНАЛИЗ)
DOI: 10.1134/S1064229318020102
Аннотация: With the help of computed X-ray microtomography with a resolution of 2.75 μm, changes in the microstructure and pore space of aggregates of 3 mm in diameter from the virgin soddy-podzolic soil (Glossic Retisol (Loamic)) in the air-dry, capillary-moistened, and frozen states after five freeze–thaw cycles were studied in a laboratory experiment. The freezing of the samples was performed at their capillary moistening. It was shown that capillary moistening of initially air-dry samples from the humus (AY), eluvial (EL), and illuvial (BT1) horizons at room temperature resulted in the development of the platy, fine vesicular, and angular blocky microstructure, respectively. The total volume of tomographically visible pores >10 μm increased by 1.3, 2.2, and 3.4 times, respectively. After freeze–thaw cycles, frozen aggregates partly preserved the structural arrangement formed during the capillary moistening. At the same time, in the frozen aggregate from the AY horizon, the total tomographic porosity decreased to the initial level of the air-dry soil. In the frozen aggregate from the EL horizon, large vesicular pores were formed, owing to which the total pore volume retained its increased values. The resistance of aggregate shape to the action of freeze–thaw cycles differed. The aggregate from the EL horizon completely lost its original configuration by the end of the experiment. The aggregate from the AY horizon displayed definite features of sagging after five freeze–thaw cycles, whereas the aggregate from the BT1 horizon preserved its original configuration.
Добавил в систему: Хайдапова Долгор Доржиевна

	ИСТИНА	Войти в систему Регистрация
	ИПМех РАН
	Главная Поиск Статистика О проекте Помощь

ИСТИНА

ИПМех РАН

The Impact of Multiple Freeze–Thaw Cycles on the Microstructure of Aggregates from a Soddy-Podzolic Soil: A Microtomographic Analysisстатья

Прикрепленные файлы