1 00:00:11,140 --> 00:00:14,060 - We're on a borrow pit along the Mississippi River 2 00:00:14,060 --> 00:00:17,480 mainline levee in Ascension Parish, Louisiana 3 00:00:17,480 --> 00:00:21,120 as part of an aquatic study for the Mississippi River 4 00:00:21,120 --> 00:00:25,370 levees Supplemental EIS for 2019. 5 00:00:25,370 --> 00:00:29,760 And this study is an extension of an earlier study 6 00:00:29,760 --> 00:00:32,170 that was done in the late 1990's and also 7 00:00:32,170 --> 00:00:33,800 part of a supplemental EIS. 8 00:00:33,800 --> 00:00:36,240 The difference today is that we have 9 00:00:36,240 --> 00:00:39,050 much better technology to help us collect these data 10 00:00:39,050 --> 00:00:42,930 and we can now let an autonomous underwater vehicle 11 00:00:42,930 --> 00:00:44,820 collect the water quality data throughout 12 00:00:44,820 --> 00:00:47,990 the entire borrow pit, whereas before we would 13 00:00:47,990 --> 00:00:51,286 have to take transects or profiles to be able to 14 00:00:51,286 --> 00:00:55,550 quantify the water quality parameters within these pits, 15 00:00:55,550 --> 00:00:59,510 and that is enabling us to much more precisely 16 00:00:59,510 --> 00:01:03,570 and comprehensively map the value of these 17 00:01:03,570 --> 00:01:07,320 aquatic areas for fishes, macro-invertebrates, 18 00:01:07,320 --> 00:01:08,453 and other organisms. 19 00:01:13,688 --> 00:01:15,410 This is part of the active floodplain 20 00:01:15,410 --> 00:01:18,670 and even though borrow pits are man-made water bodies, 21 00:01:18,670 --> 00:01:20,670 they still function because they're still 22 00:01:20,670 --> 00:01:23,160 connected to the river and they function as 23 00:01:23,160 --> 00:01:26,050 spawning areas and rearing areas for 24 00:01:26,050 --> 00:01:29,220 fishes that utilize backwaters of the Mississippi River. 25 00:01:29,220 --> 00:01:32,150 Even though the mainline Mississippi River levee 26 00:01:32,150 --> 00:01:34,430 has reduced the historic floodplain from about 27 00:01:34,430 --> 00:01:38,280 20 million acres to currently 2 million acres, 28 00:01:38,280 --> 00:01:41,800 it's still 2 million acres of very high quality habitat. 29 00:01:41,800 --> 00:01:45,850 It is the largest active connected floodplain 30 00:01:45,850 --> 00:01:47,613 in a US river system. 31 00:01:52,650 --> 00:01:55,020 One other piece of very important information 32 00:01:55,020 --> 00:01:57,550 that we're getting from this is the impact 33 00:01:57,550 --> 00:02:01,340 of big-headed carps on these areas 34 00:02:01,340 --> 00:02:05,840 because the data from previous studies were collected 35 00:02:05,840 --> 00:02:08,890 before the introduction, the widespread introduction 36 00:02:08,890 --> 00:02:11,990 of big-headed carps into this system, 37 00:02:11,990 --> 00:02:15,410 and this is sort of an indirect, big picture way 38 00:02:15,410 --> 00:02:19,046 to look at the impacts of those species 39 00:02:19,046 --> 00:02:21,196 on the fish assemblages and the 40 00:02:21,196 --> 00:02:23,870 general productivity of these backwaters. 41 00:02:23,870 --> 00:02:25,660 These are highly productive backwaters 42 00:02:25,660 --> 00:02:28,960 and they support massive growth 43 00:02:28,960 --> 00:02:32,440 and reproduction of these invasive carps, 44 00:02:32,440 --> 00:02:35,080 so understanding how that affects 45 00:02:35,080 --> 00:02:38,303 the bigger picture of the ecosystem is very important. 46 00:02:43,930 --> 00:02:46,060 - Historically, we've taken water to water quality 47 00:02:46,060 --> 00:02:49,230 measurements over time at surface and bottom, 48 00:02:49,230 --> 00:02:51,930 with the EcoMapper I can now take thousands 49 00:02:51,930 --> 00:02:54,280 of water quality points in a matter of hours. 50 00:02:54,280 --> 00:02:57,860 For example, the system that we're on today is 50 acres, 51 00:02:57,860 --> 00:03:00,090 we were able to collect the bathymetry, turbidity, 52 00:03:00,090 --> 00:03:04,300 conductivity, temperature, and pH in one swoop. 53 00:03:04,300 --> 00:03:06,810 We're not just using the EcoMapper to collect water quality, 54 00:03:06,810 --> 00:03:09,120 we're tying to fish assemblage. 55 00:03:09,120 --> 00:03:11,540 So we're going out and we're using more primitive 56 00:03:11,540 --> 00:03:14,120 technologies, gillnetting and seining, 57 00:03:14,120 --> 00:03:15,470 and then we're tying it in with some of the most 58 00:03:15,470 --> 00:03:17,960 state-of-the-art equipment in the world. 59 00:03:17,960 --> 00:03:20,995 The ERDC fish ecology team is able to translate 60 00:03:20,995 --> 00:03:25,470 these micro-habitat features into fish ecology values 61 00:03:25,470 --> 00:03:28,200 which is really a unique capability. 62 00:03:28,200 --> 00:03:30,770 - So using the points that you can map, 63 00:03:30,770 --> 00:03:33,210 as Alan said, gathers thousands of points, 64 00:03:33,210 --> 00:03:36,670 so we can take those into RTIS and create 65 00:03:36,670 --> 00:03:40,460 a continuous surface so this continual layer 66 00:03:40,460 --> 00:03:42,380 that overlays this borrow pit, 67 00:03:42,380 --> 00:03:45,450 of dissolved oxygen or chlorophyll or turbidity, 68 00:03:45,450 --> 00:03:47,460 which are important metrics to fish. 69 00:03:47,460 --> 00:03:49,650 Focusing on dissolved oxygen, 70 00:03:49,650 --> 00:03:52,420 the thing that we can do is if we look at that 71 00:03:52,420 --> 00:03:55,050 point cloud of dissolved oxygen and look for 72 00:03:55,050 --> 00:03:58,720 a range of DO that's important to us, specific fish species, 73 00:03:58,720 --> 00:04:01,010 or to the fish assemblage as a whole, 74 00:04:01,010 --> 00:04:03,640 we can estimate the volume of water 75 00:04:03,640 --> 00:04:05,760 where the dissolved oxygen is high enough 76 00:04:05,760 --> 00:04:08,690 to support those fish that we're interested in. 77 00:04:08,690 --> 00:04:11,480 That can then be translated into management measures. 78 00:04:11,480 --> 00:04:13,730 We can change the connectivity of the borrow pit 79 00:04:13,730 --> 00:04:16,070 to allow fresh water to flow in and create 80 00:04:16,070 --> 00:04:19,010 a little bit of flow which will improve the DO. 81 00:04:19,010 --> 00:04:22,030 We can add more tree cover along the outside edges 82 00:04:22,030 --> 00:04:24,310 of the borrow pit because that tree cover 83 00:04:24,310 --> 00:04:27,700 will shade the borrow pit that algae won't grow as fast 84 00:04:27,700 --> 00:04:30,790 and that algae, although it produces dissolved oxygen 85 00:04:30,790 --> 00:04:34,420 during the day, at night it sucks all that oxygen up 86 00:04:34,420 --> 00:04:36,645 and then there's no oxygen for the fish. 87 00:04:36,645 --> 00:04:38,473 So there's specific management measures 88 00:04:38,473 --> 00:04:40,810 we can implement in this borrow pit, 89 00:04:40,810 --> 00:04:43,820 but also throughout the Mississippi floodplain as a whole, 90 00:04:43,820 --> 00:04:46,537 from this data we're gathering from the EcoMapper. 91 00:04:51,526 --> 00:04:55,090 - One of the big benefits to doing this study is that 92 00:04:55,090 --> 00:04:58,150 not only are we repeating a study 93 00:04:58,150 --> 00:05:01,640 from 20 years ago so it's directly comparable, 94 00:05:01,640 --> 00:05:04,280 we're also collecting additional data 95 00:05:04,280 --> 00:05:06,760 that allows us to input these water bodies 96 00:05:06,760 --> 00:05:09,090 into our larger ecohydrology database, 97 00:05:09,090 --> 00:05:12,840 so the larger study of the connectivity 98 00:05:12,840 --> 00:05:14,570 of these water bodies is still lie within 99 00:05:14,570 --> 00:05:17,180 the active floodplain to the Mississippi River 100 00:05:17,180 --> 00:05:19,930 and assess their value on a larger scale. 101 00:05:19,930 --> 00:05:23,400 So our ecohydrology study is looking at 102 00:05:23,400 --> 00:05:26,730 the frequency of connection of water bodies within 103 00:05:26,730 --> 00:05:30,090 the active floodplain that are at different elevations, 104 00:05:30,090 --> 00:05:32,530 so depending on your hydrograph, 105 00:05:32,530 --> 00:05:35,180 different water bodies will connect to the river, 106 00:05:35,180 --> 00:05:38,600 to the main channel, for a different period of time, 107 00:05:38,600 --> 00:05:42,110 a different time of the year and somehow flow through, 108 00:05:42,110 --> 00:05:44,610 and some are backwater connections only. 109 00:05:44,610 --> 00:05:46,930 And fishes and macro-invertebrates, and other organisms 110 00:05:46,930 --> 00:05:50,200 utilize all of those different habitats differently. 111 00:05:50,200 --> 00:05:54,330 So, understanding that is a way to get a bigger picture 112 00:05:54,330 --> 00:05:57,110 and a more comprehensive picture of the 113 00:05:57,110 --> 00:05:59,063 greater Mississippi River ecosystem. 114 00:06:00,636 --> 00:06:03,136 (outro music)