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<br />. <br /> <br />. <br /> <br />, <br /> <br />\., 0762 <br /> <br />water supply from the average existing supply of 65 percent to 95 percent, <br /> <br /> <br />provided the ultimate plan is adopted as set forth in their report. The <br /> <br /> <br />monthly reservoir operation study indicates that the reservoir would be <br /> <br /> <br />empty about 5.7 percent of the time with water shortages occurring in 1934, <br /> <br /> <br />1935, 1936, 1937, 1939 and 1940. The longest period of consecutive <br /> <br /> <br />monthly shortages occurred in 1940 for a 5-month period, June through <br /> <br /> <br />October. The Bureau of Reclamation report on Trinidad Reservoir, and the <br /> <br /> <br />reservoir oper'"tion studies for the period 1925-1949 are included in <br /> <br /> <br />appendix D. <br /> <br /> <br />44. SediwG:1G sources. - The mountains are not an important source <br /> <br /> <br />of sediment; but there are debris cones in the lower reaches of the <br /> <br /> <br />tributaries and there is evidence of considerable lateral erosion. The <br /> <br /> <br />entire stream sys'~e;n moves an appreciable bed load as evidenced by the <br /> <br /> <br />wide, flat stream bed cOffiposed of sand and coarse material to cobble sizes. <br /> <br /> <br />Degradation of the 'stream bed occurs during flood flows, but aggradation <br /> <br /> <br />of the bed occurs during smaller flows. The steep slope of the river <br /> <br /> <br />above Trinidad, lack of vegetative growth in the channel, and the abun- <br /> <br /> <br />dance of bed material is also conducive to bed load movement. <br /> <br /> <br />L6. Sediment sampling. - From 1940 to 1943, suspended sediment <br /> <br /> <br />samples were obtained intermittently from the Purgatoire River at Trinidad, <br /> <br /> <br />Colorado. Since 1943, sampling has been continued at the rate of about <br /> <br /> <br />two samples per week at this station from 1 April to 30 September each <br /> <br /> <br />year, and additional samples have been taken dl~ing flood stages. Only <br /> <br /> <br />intermittent samples are obtained during the winter. Samples of bed load <br /> <br /> <br />are not obtained; therefore, only a preliminary estimate of the bed load <br /> <br /> <br />can be made. <br /> <br /> <br />46. Sediment volume at Trinidad. - Suspended sediment volume for <br /> <br /> <br />the sampling period was computed by plotting the stream discharge from <br />the recording gage; plotting the sampled sediment in percent by weight; <br /> <br />35 <br /> <br />APPENDIX B <br /> <br />. <br /> <br />