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<br />~ <br /> <br />1:'- <br />~ <br />;,'J <br />(e.:) <br />"'-, <br />1..... <br /> <br />D, Co.parison with Salt Marsh Habitats <br /> <br />Certain characte~istics of the ~egion are similar to those <br />within salt marsh habitats. These include water quality and <br />wind velocity. Other cha~acteristics are distinctly diffe~ent, <br />These include insolation, temperature, humidity, and <br />p~ecipitation, <br /> <br />1. Water Quality <br /> <br />Table IV gives the composition of major elements within <br />seawater, The propo~tionate composition of most ions is nearly <br />identical to Glenwood Springs water. Magnesium is approximately <br />seven to eight times as abundant in seawate~, and bicarbonate is <br />about fivefold higher in proportionate concentrations within <br />Glenwood Springs water, Glenwood Springs has a TDS of 53% of <br />this seawater formulation. <br /> <br />The significance of this is that coastal salt marsh plants <br />should have little difficulty adjusting to the ionic composition <br />of Glenwood Springs water, <br /> <br />TABLE IV: COMPOSTIO~ OF SEAWATER (Hanson, 1974) <br /> <br />Ion Concentration <br />mg/l me/l <br /> <br />Na+ <br />K+ <br />Ca?+ <br />Mg-!-? <br /> <br />10,760 <br />387 <br />413 <br />1,294 <br /> <br />468,03 <br />9,90 <br />20.61 <br />106,45 <br /> <br />Total cations <br /> <br />604,99 <br /> <br />HC~3 <br />CI <br />= <br />S04 <br />Total anions (Major) <br /> <br />149 <br />19,353 <br />2,712 <br /> <br />2.44 <br />545,88 <br />56,46 <br /> <br />604,78 <br /> <br />TOTAL <br /> <br />35,068 <br /> <br />2, Wind Velocity <br /> <br />As will be discussed in the next section, wind velocity is an <br />important determinant of both rates of transpiration and <br />growth, A fairly low speed is required to provide sufficient <br />air flow to break down the boundrary layer at the ai~-leaf <br />surface interface to promote good gas exchange, Good gas <br />exchange, in tu~n, leads to improved productivity and greater <br />water loss. <br /> <br />9. <br />