| 000 -LEADER |
|---|
| fixed length control field |
01369pab a2200169 454500 |
| 008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION |
|---|
| fixed length control field |
180718b1999 xxu||||| |||| 00| 0 eng d |
| 100 ## - MAIN ENTRY--PERSONAL NAME |
|---|
| Personal name |
Satsangi, Gur Sumiran et al. |
| 245 ## - TITLE STATEMENT |
|---|
| Title |
Dry deposition at five sites of Western U.P. |
| 260 ## - PUBLICATION, DISTRIBUTION, ETC. |
|---|
| Date of publication, distribution, etc. |
1999 |
| 300 ## - PHYSICAL DESCRIPTION |
|---|
| Extent |
p.217-28 |
| 362 ## - DATES OF PUBLICATION AND/OR SEQUENTIAL DESIGNATION |
|---|
| Dates of publication and/or sequential designation |
Jul |
| 520 ## - SUMMARY, ETC. |
|---|
| Summary, etc. |
Dry deposition rates of major water soluble species F,C1, No3,SO4,NH4, Na, K, Ca and Mg were estimated at Dayalbagh, Gopalpura, Etah, Budaun and Mainpuri, F, C1,No3 and SO4 were measured by Ion Chromatography (Dionex), NH4, colorimetrically, and Na, K, Ca and Mg were determined by Atomic Absorption Spectometry. Deposition rates of the crustal components (Ca, Na and K) wer higher due to their large mass median diameter. The dry deposition rates of NO3 and SO4 were also similiar to crustal components suggesting a common origin. Spatial variations in dry deposition of ions were determined by calculating maximum/minimum ratio. On this basis the ions could be divided into two classes; low (<2) and high (>3). Low class included the crustal components showing minimum variability while NO3 and SO4 showed spatial variation. Deposition rates of ions are more in winter than summer at the selected sites. - Reproduced |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
|---|
| Topical term or geographic name entry element |
Arid zones - India - Uttar Pradesh |
| 650 ## - SUBJECT ADDED ENTRY--TOPICAL TERM |
|---|
| Topical term or geographic name entry element |
Arid zones |
| 773 ## - HOST ITEM ENTRY |
|---|
| Main entry heading |
Indian Journal of Environmental Health |
| 909 ## - |
|---|
| -- |
43735 |
