About water regime of the eastern Shirvan lands

Font:      

Summary
It is shown in the article that we came to conclusion that while characterizing lands of hospital No 2 in Shirvan the water dynamics of the lands depend on climate condition, changing of the level of the underground waters, artificial irrigation, mechanical structure of the land and type of the plant cover.
Annual course of the water dynamics of the land showed that amount of the dampness of the land where a root of plant located changes depending on variety of land type in zonal form. Being as rule in of water dynamics of separate land types some changes were defined. So, in connection with climate condition 40-60 cm upper layer of all types of land are very variable.
It was defined that there is permanent dry layer in the mid of some land profiles that we specify.



Read: 2119

Comments: 1
Please wright your opinion to article and view others comments

Books

Salinization of lands in Shirvan plain and researches of struggle with it Salinization of lands in Shirvan plain and researches of struggle with it
Land improvement of mil plain Land improvement of mil plain
Fast land improvement of loamy saline lands of Azerbaijan Fast land improvement of loamy saline lands of Azerbaijan
Lands with dealluvial form of salinization and matters of its improvement Lands with dealluvial form of salinization and matters of its improvement
Dealluvial saline lands in plains of Azerbaijan Dealluvial saline lands in plains of Azerbaijan
Saline lands in Azerbaijan and its improvement Saline lands in Azerbaijan and its improvement
My mountains My mountains