Elastic Properties of Natural Sea Surface Films Incorporated with Solid Dust Particles: Model Baltic Sea Studies

<table class="table-group" id="tab2"><tr><td><table class="table"><tr><td class="thead-hr" colspan="5"><hr/></td></tr><tr class="thead"><td align="center" colspan="5">CA determination technique</td></tr><tr class="thead"><td align="left">Sample/phase</td><td align="center">Sessile drop</td><td align="center">Isotherm derived from (<a href="https://static.hindawi.com/articles/ijocean/volume-2012/638240/figures/#EEq10">8</a>)</td><td align="center">Microscope technique</td><td align="center">Thin layer wicking technique</td></tr><tr><td class="thead-hr" colspan="5"><hr/></td></tr><tr><td align="left">Talc<sup>W</sup></td><td align="center" rowspan="2">108.6 ± 6.8</td><td align="center">110.9 ± 6.5</td><td align="center">88.8 ± 5.4</td><td align="center">80.3 ± 4.8<br/>(<svg height="13.95" id="M155" style="vertical-align:-0.1638pt" version="1.1" viewbox="0 0 96.900002 13.95" width="96.900002" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
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<g transform="matrix(.012,-0,0,-.012,7.238,5.525)"><path d="M471 153q-22 -15 -61 -13q-25 31 -45.5 49.5t-56.5 41.5q4 -71 28 -134q-17 -33 -42 -46q-24 12 -42 46q24 63 28 134q-36 -23 -56.5 -41.5t-45.5 -49.5q-36 -2 -61 13q0 28 19 59q65 10 130 43q-65 33 -130 43q-19 31 -19 59q22 15 61 13q25 -31 45.5 -49.5t56.5 -41.5
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</svg>)</td></tr><tr><td align="left">Talc<sup>S</sup></td><td align="center">112.0 ± 6.7</td><td align="center">93.9 ± 5.7</td><td align="center">86.7 ± 5.2</td></tr><tr><td align="left" colspan="5"><hr/></td></tr><tr><td align="left">Microsphere<sup>W</sup></td><td align="center" rowspan="2">99.4 ± 6.1</td><td align="center">88.3 ± 5.3</td><td align="center">62.0 ± 4.2</td><td align="center">78.0 ± 4.6<br/>(<svg height="13.95" id="M156" style="vertical-align:-0.1638pt" version="1.1" viewbox="0 0 14.9 13.95" width="14.9" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
<g transform="matrix(.017,-0,0,-.017,.062,13.688)"><path d="M393 379q-9 -16 -28 -29q-15 -10 -23 -2q-19 19 -36 19q-21 0 -52 -38q-57 -72 -82 -126l-40 -197q-23 -3 -75 -18l-7 7q49 196 74 335q7 43 -2 43q-7 0 -30 -14.5t-47 -37.5l-16 23q37 42 82 73t67 31q41 0 15 -113l-11 -50h4q41 71 85 117t77 46q29 0 45 -26
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<g transform="matrix(.012,-0,0,-.012,7.238,5.525)"><path d="M471 153q-22 -15 -61 -13q-25 31 -45.5 49.5t-56.5 41.5q4 -71 28 -134q-17 -33 -42 -46q-24 12 -42 46q24 63 28 134q-36 -23 -56.5 -41.5t-45.5 -49.5q-36 -2 -61 13q0 28 19 59q65 10 130 43q-65 33 -130 43q-19 31 -19 59q22 15 61 13q25 -31 45.5 -49.5t56.5 -41.5
q-4 71 -28 134q17 33 42 46q24 -12 42 -46q-24 -63 -28 -134q36 23 56.5 41.5t45.5 49.5q36 2 61 -13q0 -28 -19 -59q-65 -10 -130 -43q65 -33 130 -43q19 -31 19 -59z" id="x2217"></path></g>
</svg> = 1301.1<svg height="0.125" id="M157" style="vertical-align:-0.0pt" version="1.1" viewbox="0 0 2.9625001 0.125" width="2.9625001" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
</svg>nm)</td></tr><tr><td align="left">Microsphere<sup>S</sup></td><td align="center">92.2 ± 5.5</td><td align="center">68.1 ± 4.8</td><td align="center">83.0 ± 4.9</td></tr><tr><td align="left" colspan="5"><hr/></td></tr><tr><td align="left">Combustion dust<sup>W</sup></td><td align="center" rowspan="2">120.6 ± 7.1</td><td align="center">117.7 ± 6.9</td><td align="center">116.9 ± 6.0</td><td align="center">124.2 ± 8.3<br/>(<svg height="13.95" id="M158" style="vertical-align:-0.1638pt" version="1.1" viewbox="0 0 14.9 13.95" width="14.9" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
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<g transform="matrix(.012,-0,0,-.012,7.238,5.525)"><path d="M471 153q-22 -15 -61 -13q-25 31 -45.5 49.5t-56.5 41.5q4 -71 28 -134q-17 -33 -42 -46q-24 12 -42 46q24 63 28 134q-36 -23 -56.5 -41.5t-45.5 -49.5q-36 -2 -61 13q0 28 19 59q65 10 130 43q-65 33 -130 43q-19 31 -19 59q22 15 61 13q25 -31 45.5 -49.5t56.5 -41.5
q-4 71 -28 134q17 33 42 46q24 -12 42 -46q-24 -63 -28 -134q36 23 56.5 41.5t45.5 49.5q36 2 61 -13q0 -28 -19 -59q-65 -10 -130 -43q65 -33 130 -43q19 -31 19 -59z" id="x2217"></path></g>
</svg> = 695.7<svg height="0.125" id="M159" style="vertical-align:-0.0pt" version="1.1" viewbox="0 0 2.9625001 0.125" width="2.9625001" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
</svg>nm)</td></tr><tr><td align="left">Combustion dust<sup>S</sup></td><td align="center">120.1 ± 7.2</td><td align="center">126.2 ± 6.8</td><td align="center">128.7 ± 4.6</td></tr><tr class="table-tr"><td colspan="5"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

Contact angles (CA) of studied mineral dust particles with distilled (W) and original sea water (S) derived by means of different techniques. <svg height="13.95" id="M154" style="vertical-align:-0.1638pt" version="1.1" viewbox="0 0 14.9 13.95" width="14.9" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink">
<g transform="matrix(.017,-0,0,-.017,.062,13.688)"><path d="M393 379q-9 -16 -28 -29q-15 -10 -23 -2q-19 19 -36 19q-21 0 -52 -38q-57 -72 -82 -126l-40 -197q-23 -3 -75 -18l-7 7q49 196 74 335q7 43 -2 43q-7 0 -30 -14.5t-47 -37.5l-16 23q37 42 82 73t67 31q41 0 15 -113l-11 -50h4q41 71 85 117t77 46q29 0 45 -26
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<g transform="matrix(.012,-0,0,-.012,7.238,5.525)"><path d="M471 153q-22 -15 -61 -13q-25 31 -45.5 49.5t-56.5 41.5q4 -71 28 -134q-17 -33 -42 -46q-24 12 -42 46q24 63 28 134q-36 -23 -56.5 -41.5t-45.5 -49.5q-36 -2 -61 13q0 28 19 59q65 10 130 43q-65 33 -130 43q-19 31 -19 59q22 15 61 13q25 -31 45.5 -49.5t56.5 -41.5
q-4 71 -28 134q17 33 42 46q24 -12 42 -46q-24 -63 -28 -134q36 23 56.5 41.5t45.5 49.5q36 2 61 -13q0 -28 -19 -59q-65 -10 -130 -43q65 -33 130 -43q19 -31 19 -59z" id="x2217"></path></g>
</svg>: pore radius.

International Journal of Oceanography

tab2

Table 2

Table 2: Elastic Properties of Natural Sea Surface Films Incorporated with Solid Dust Particles: Model Baltic Sea Studies 