Refine your search
Collections
Co-Authors
A B C D E F G H I J K L M N O P Q R S T U V W X Y Z All
Mathur, K. C.
- Soils of South Kheri Forests of Uttar Pradesh
Abstract Views :184 |
PDF Views:0
Authors
Source
Indian Forester, Vol 116, No 6 (1990), Pagination: 479-486Abstract
Eight different soils were recognized in South Kheri forests on the basis of diffence in their characteristics. The soils are developed on alluvial sediments and are more or less young with marks of pedogenesis either faint or lacking. Sand constitutes the bulk of the solum invariably with varying amounts of silt and clay in the pedons and manifest their properties accordingly. Grasses appear to be the initial colonizers of the depositional surfaces and with advancement in pedogenesis woodland replaced grasslands in the process or ecological succession. They do not appear to have atained equilibrium with their environments so far and are still in dynamic state.- Clay Minerals in the Soils of South Kheri Forests, Uttar Pradesh
Abstract Views :160 |
PDF Views:0
Authors
Source
Indian Forester, Vol 115, No 8 (1989), Pagination: 555-559Abstract
X-ray diffraction of selected soil clay of South Kheri forests of Uttar Pradesh brings out kaolinite as the dominant silicate mineral, both at the surface as well as the subsurface of all the pedons. In addition, small amounts of goethite, gibbsite and integrated micaceous minerals are also identified in the clay fractions. An occurrence of some vermiculite only in the three pedons under natural sal (Shorea robusta), which decreased at the subsurface, may perhaps be a peculiar coincidence only as no tangible explanation exists.- Sand Minerals on the Soils of South Kheri Forests' Uttar Pradesh
Abstract Views :242 |
PDF Views:0
Authors
Source
Indian Forester, Vol 114, No 12 (1988), Pagination: 874-881Abstract
Mineralogical study of the fine sand fraction of ten typical soils of 'South Kheri forests of Uttar Pradesh brings out that quartz is the preponderant detrital mineral in all these alluvial soils followed by mica which is higher in lower depths' especially the muscovite type. The heavy minerals which are present in small quantities' include mainly chlorite' iron-ores and tourmaline' and in very small quantities zircon' sphene' staurolite' apatite' garnet' bornblende' kyanite and epidote. Petrographic examination revealed that excepting quartz' which is in abundance throughout the depth of the pedons' no other mineral' light or heavy' shows any definite trend of distribution along the depths of the pedons. No definite relationship appears to exist between the nature of these skeletal minerals and growth' development and distribution of the vegetation of the area.- Fatty Oils from Oilseeds of Forest Origin as Antibacterial agents
Abstract Views :187 |
PDF Views:0
Authors
Source
Indian Forester, Vol 113, No 4 (1987), Pagination: 297-299Abstract
Fatty oils extracted from seed of Cassia tora Linn., Wrightia tomentosa Roem &Schult., Viburnum coriaceum Blume, Michelia champaca Linn., Pongamia pinnato and Azadirachta indica A Juss., have been tested in vitro against five species of bacteria i.e. Bacillus pumilus Gottheil, Bacillus subtilis Cohn, Salmonella typhosa (Zopf) white syn. Salmonella typhi Warren and Scott., S paratyphi (Kayer) Casteliani and Chalmers and Micrococcus pyogens var. albus (Rosenbach, Schroeten) Syn. Staphylococcus albus Rosenbach. Present investigations reveal that all the above mentioned fatty oils have potent antibacterial efficay against Bacillus subtilis, Salmonella typhosa and S paratyphi.- Effect of Tulsi (Ocimum sanctum Linn) on Clinical and Biochemical Parameters of Metabolic Syndrome
Abstract Views :616 |
PDF Views:581