Rheological Features of the Coagulative Structure of Northern Taiga Peaty Podzolic Semi_Gley Soils of the European Northeast

Авторы: Khaydapova D.D., Kholopov Yu V., Zaboeva I.V., Lapteva E.M.
Журнал: Moscow University Soil Science Bulletin
Том: 69
Номер: 1
Год издания: 2014
Издательство: Allerton Press Inc.
Местоположение издательства: United States
Первая страница: 17
Последняя страница: 22
Оригинальные версии: РЕОЛОГИЧЕСКИЕ ОСОБЕННОСТИ КОАГУЛЯЦИОННОЙ СТРУКТУРЫ СЕВЕРОТАЕЖНЫХ ТОРФЯНИСТО-ПОДЗОЛИСТО-ГЛЕЕВАТЫХ ПОЧВ ЕВРОПЕЙСКОГО СЕВЕРО-ВОСТОКА
DOI: 10.3103/S0147687414010050
Аннотация: The results of rheological studies using a MCR 302 modular research rheometer of soil pastes of northern taiga peaty podzolic semigley soils are presented. It was found that their coagulative structure has weak structural links. They are little resistant to mechanical stress and their stability decreases in the direction from the northern to the extreme northern taiga by about two times. The strongest coagulative links between soil particles characterize the horizons with increased organic contents and the horizons that are transient in terms of granulometric composition, which lie at the border where light deposits shift heavier ones. Keywords: northern taiga soils, structure formation, rheology
Добавил в систему: Хайдапова Долгор Доржиевна

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

ИСТИНА