ON THE ABILITY OF ATMOSPHERIC VAPOROUS WATER TO CONDENSATE WITHIN THE SOIL ON THE BACKGROUND OF THERMAL BALANCE AND EXPERIMENTAL MATERIALS

On the basis of experimental works considering the condensation of vaporous atmospheric water within the soil, A.A. Rode concluded that the summer night water condensation in dry surface soil layers with volume 0.1-0.2 mm is a common phenomenon. Along with that, the possibility of atmospheric water...

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Hlavní autor:	N. F. Kulik
Médium:	Artigo
Jazyk:	Russo
Vydáno:	V.V. Dokuchaev Soil Science Institute 2016-05-01
Edice:	Бюллетень Почвенного института им. В.В. Докучаева
Témata:	конденсация атмосферной влаги парожидкостный поток термоградиентный перенос влаги зона аэрации грунтовые воды пески condensation of atmospheric water vapour and water flow thermal-gradient water transfer aeration zone ground waters sands
On-line přístup:	https://bulletin.esoil.ru/jour/article/view/80
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