Zobrazeno 1 - 10
of 31
pro vyhledávání: '"D. B. Das"'
Publikováno v:
Waste and Biomass Valorization. 14:1369-1389
Autor:
F. M. Pelicice, D. B. das Chagas
Publikováno v:
Community Ecology. 19:211-222
Fire is a constitutive ecological force in savanna ecosystems, but few studies have monitored its short-term effects on plant community dynamics. This study investigated changes in plant diversity in the South American savanna (Cerrado) after severe
Autor:
Guha, P. C., Gupta, D. B. Das
Publikováno v:
Current Science, 1943 Apr 01. 12(4), 120-120.
Externí odkaz:
https://www.jstor.org/stable/24210514
Publikováno v:
Proceedings of Indian National Science Academy, Vol 22, Iss 6A (2015)
Pentoses in Jute α-Cellolose, Part I
Publikováno v:
Proceedings of Indian National Science Academy, Vol 21, Iss 4A (2015)
Paper Chromatographic Study of Jute Holocellulose
Publikováno v:
Annals of Tropical Medicine & Parasitology. 93:109-118
Autor:
Chagas, D. B. das, Pelicice, F. M.
Publikováno v:
Community Ecology; 2018, Vol. 19 Issue 3, p211-222, 12p
Autor:
D B, Das, V, Nassehi
Publikováno v:
Water science and technology : a journal of the International Association on Water Pollution Research. 45(9)
The interfaces between free (e.g., groundwater) and porous (e.g., soil) flow zones in the subsurface represent important transition zones across which many important transfer/exchange processes occur. The understanding of these interactive phenomena
Publikováno v:
Water science and technology : a journal of the International Association on Water Pollution Research. 43(7)
The tidal hydrodynamics and effluent distribution in estuaries involve a complicated range of solute transport phenomena modelled by partial differential equations. Therefore, the quantitative estimation of the risks of water and soil contamination o
Autor:
D B, Das, V, Nassehi
Publikováno v:
Water science and technology : a journal of the International Association on Water Pollution Research. 43(7)
Free and porous flow of water in lands often occurs in combination under different physical circumstances. To model such configurations, open and porous flow regions need to be studied independently and also to integrate them through well-posed mathe