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  <controlfield tag="008">180718b1999   xxu||||| |||| 00| 0 eng d</controlfield>
  <datafield tag="100" ind1=" " ind2=" ">
    <subfield code="a">Satsangi, Gur Sumiran et al.</subfield>
  </datafield>
  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">Dry deposition at five sites of Western U.P.</subfield>
  </datafield>
  <datafield tag="260" ind1=" " ind2=" ">
    <subfield code="c">1999</subfield>
  </datafield>
  <datafield tag="300" ind1=" " ind2=" ">
    <subfield code="a">p.217-28</subfield>
  </datafield>
  <datafield tag="362" ind1=" " ind2=" ">
    <subfield code="a">Jul</subfield>
  </datafield>
  <datafield tag="520" ind1=" " ind2=" ">
    <subfield code="a">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 (&lt;2) and high (&gt;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</subfield>
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  <datafield tag="650" ind1=" " ind2=" ">
    <subfield code="a">Arid zones - India - Uttar Pradesh</subfield>
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  <datafield tag="650" ind1=" " ind2=" ">
    <subfield code="a">Arid zones</subfield>
  </datafield>
  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="a">Indian Journal of Environmental Health</subfield>
  </datafield>
  <datafield tag="909" ind1=" " ind2=" ">
    <subfield code="a">43735</subfield>
  </datafield>
  <datafield tag="999" ind1=" " ind2=" ">
    <subfield code="c">43735</subfield>
    <subfield code="d">43735</subfield>
  </datafield>
  <datafield tag="952" ind1=" " ind2=" ">
    <subfield code="0">0</subfield>
    <subfield code="1">0</subfield>
    <subfield code="4">0</subfield>
    <subfield code="7">0</subfield>
    <subfield code="a">IIPA</subfield>
    <subfield code="b">IIPA</subfield>
    <subfield code="d">2018-07-19</subfield>
    <subfield code="h">Volume no: 41, Issue no: 3</subfield>
    <subfield code="p">AR44134</subfield>
    <subfield code="r">2018-07-19</subfield>
    <subfield code="w">2018-07-19</subfield>
    <subfield code="y">AR</subfield>
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