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t <br />?J <br />may have always had available to them portions of the pond containing <br />t adequate levels of dissolved oxygen. Water clarity in West Pond was <br />usually high, allowing us to view the pond bottom during most of the year <br />' (Fig. 7). However, after fertilizing the pond in early May 1987, algal <br />growth increased and Secchi disk visibility dropped to 0.8 m. Rapid <br />decomposition of organic matter after cessation of the algae bloom proba- <br />bly caused the depletion of oxygen. Clarity and DO again increased in mid <br />to late September. <br />t <br />I <br />t <br />1 <br />Limited winterkill was detected at ice-out in early 1988. We collected a <br />total of 25 dead squawfish from the surface and bottom of the pond during <br />3-9 March. Water samples collected from the north and south ends of the <br />pond at two depths (mid- and bottom) on 15 March revealed relatively high <br />levels of hydrogen sulfide (0.002-0.014 mg/L). Though the levels we <br />detected in West Pond with our limited sampling effort were lower than the <br />3.5 <br />r. <br />1 <br />1 <br />1 <br />t <br />1 <br />1 <br />3 <br />E <br />2.5 <br />I- <br />a <br />w 2 <br />0 <br />U 1.5 <br />U <br />W <br />co 1 <br />0.5 <br />0 l I I 1 I 1 I I 1 I I I I 1 I I I 1 1 1 I I I <br />S 0 N D J F M A M J J A S O N D J F M A M J J A S O <br />1986 1987 1988 <br />---- FISH CHALET - HUMPHREY - WEST <br />Figure 7. Water clarity, as measured by Secchi disk visibility, in three <br />study ponds, 1986-88. <br />29