Laserfiche WebLink
<br />0185J <br /> <br />Test/nx Ia.~er-bast'd senwn for continUOUS In SIlU monilorHlg o[suv-.ended .w'd,menl 5 <br /> <br />-lISST2S8POiI\lT I.lEASUREII.IENT (NO C....1.I8AATION) <br />o CROSS-SECTlONAU. Y I,..TEGAATEO WITH o..n SAMPLER <br />-OISCHARGEOI' WATER <br /> <br />"'" <br /> <br /> <br />.., <br /> <br />r <br /> <br />o <br />300 ~ <br />, <br />> <br />. <br />o <br />m <br /> <br />z <br />g 11.lOO:l <br />~ <br />. <br />z <br />. <br />o <br />z <br />o <br />o <br />. <br />z <br />. <br />, <br />" <br />. <br />. <br />" <br />. <br />o <br />z <br />~ <br />. <br />il <br /> <br />"'" <br /> <br />100 '3 <br />,- <br />. <br /> <br />"'" <br /> <br />~<<> <br /> <br />o <br /> <br />ussr OUT OF RANGE <br /> <br />" <br /> <br />- - - - - ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ ~ <br />~ ~ ~ ~ ~ . . . . . . . . . . . . . <br />~ ~ ~ ~ ~ ~ ~ 6 ~ 6 ~ 6 6 6 0 ~ ~ ~ <br />= ~ 0 = 0 _ _ _ _ _ _ _ _ _ _ _ _ <br /> <br />~ ~ <br />re ::; <br />e 2 <br /> <br />Fig. 5 Comparison of local ML~pended+sediment concenlrallons (1.3-250 j.Im) <br />measured allhe Grand Canyon gauge using L1SST-25 and [)..77 bag ~mp[er during <br />the mulli.....eek fall 2001 lest. DlliCharge dala are from the Gr.md Canyon gauge. <br /> <br />". <br /> <br />L1SST-25 provided the most compelling results as to how well these optical <br />Instruments perform during continuous deployments (Fig. 5). Even during September <br />200t. when the LlSST-25 was technically oUl-of-rnnge (laser transmission <2(010), <br />these non-calibrdted data generally tracked the 0-77 samples. <br />Although the non-calibrated test results from the LlSST -25 compare well with <br />cross-section measurements for total concentration (once the volume to mass <br />conversion was made, Fig. 5). the LlSST-25 provides no possibility for separating <br />measurements of sand from finer panicles (the sand split is made at 63 11m). This <br />L1SST -25 limitation presents a serious shortcoming for monitoring deploymt'nts where <br />sand transpon is of primary concern. such as the Colorado River. During the 2002 field <br />tests, the manufacturer developed a L1SST -25 lirnlware upgrade to segregate sand <br />from liner-panicle data and made it available for testing (L25X). The July 2002 sand <br />concentrations derived from the L25X compared very well with cableway sample data <br />(R' = 0.86). <br />During relatively brief periods when the river below the da.m becomes greatly <br />enriched with tine sediment from tributary inputs, LlSST overestimates the <br />concentration of flOe panicles (Fig. 5). Such errors occur owing to multiple scallenng <br />associated with abundant fines. a phenomenon that tends to bias counts on the outt'r <br />rings of the detector array. Multiple scallenng has been identified as a significant <br />source of concentration error when laser transmission falls below 20% (Agrawal & <br />POllsmith. 2001). To monitor such periods. a method was devised that allowed the <br />L1SST to electronically control a programmable automated pumping sampler. The <br />protocol is as follows: when L1SST measures laser transmission below the 20~.o <br />