fix FisherTwining2024b abstract entry

README.md

@@ -59,12 +59,12 @@ help(package = "inlpubs")
 
 ## Authors
 
--   Jason C. Fisher (ORCID iD
-    [0000-0001-9032-8912](https://orcid.org/0000-0001-9032-8912))
--   Kerri C. Treinen (ORCID iD
-    [0000-0003-0645-6810](https://orcid.org/0000-0003-0645-6810))
--   Allison R. Trcka (ORCID iD
-    [0000-0001-8498-4737](https://orcid.org/0000-0001-8498-4737))
+- Jason C. Fisher (ORCID iD
+  [0000-0001-9032-8912](https://orcid.org/0000-0001-9032-8912))
+- Kerri C. Treinen (ORCID iD
+  [0000-0003-0645-6810](https://orcid.org/0000-0003-0645-6810))
+- Allison R. Trcka (ORCID iD
+  [0000-0001-8498-4737](https://orcid.org/0000-0001-8498-4737))
 
 ## Point of Contact
 

data-raw/publications/pubs-2024.json

@@ -33,7 +33,7 @@
       "doi": "10.5066/P9V6VCBO",
       "textVersion": "Fisher, J.C., and Twining, B.V., 2024, mlms—Multilevel Monitoring System (MLMS) data storage and processing for the U.S. Geological Survey Idaho National Laboratory Project Office: U.S. Geological Survey software release, R package, https://doi.org/10.5066/P9V6VCBO."
     },
-    "abstract": "The [R](https://www.r-project.org/) package **mlms** is used to store and process Multilevel Monitoring System (MLMS) data for wells in the U.S. Geological Survey (USGS) aquifer-monitoring network, Idaho National Laboratory (INL), Idaho. Supported by the U.S. Department of Energy (DOE), the USGS collected `r npress` discrete hydraulic head measurements at various depths from `r nwells` wells in the eastern Snake River Plain (ESRP) aquifer from `r dt_range_press[1]`--`r dt_range_press[2]`. These measurements were derived from data on fluid pressure, fluid temperature, and atmospheric pressure. Each well was equipped with an MLMS, which included valved measurement ports, packer bladders, casing segments, and couplers. The MLMS allowed monitoring at `r nzones` hydraulically-isolated depth intervals, reaching depths as great as `r depth_max` feet below the land surface. Additionally, `r nsamples` groundwater samples were collected from these wells from `r dt_range_sample[1]`--`r dt_range_press[2]`, and analyzed for a wide range of chemical and physical parameters. Many investigations have assessed the geology and hydrology of the ESRP aquifer at and near the INL, with a comprehensive listing of USGS Idaho National Laboratory Project Office ([INLPO]) publications available [online]. Fisher and Twining (2011) documented the use of Multilevel Monitoring Systems to examine hydraulic head and temperature in six wells from 2007--2008. Subsequent expansions included nine wells (Twining and Fisher, 2012), 11 wells (Twining and Fisher, 2015), and 12 wells (Twining and others, 2021). Various studies have documented water chemistry at different depths in the ESRP aquifer, with summaries of water-quality data collected from 2005--2008 provided by Bartholomay and Twining (2010), 2009--2011 provided by Davis and others (2013), 2009--2013 provided by Bartholomay and others (2015), 2012--2015 provided by Bartholomay and others (2017), and 2014--2018 provided by Twining and others (2021). A tracer study by Bartholomay and others (2013) examined whether drilling fluids could remain in the MLMS wells and found that the tracer moved out of the formation for most of the monitoring zones analyzed."
+    "abstract": "The R package mlms is used to store and process Multilevel Monitoring System (MLMS) data for wells in the U.S. Geological Survey (USGS) aquifer-monitoring network, Idaho National Laboratory (INL), Idaho. Supported by the U.S. Department of Energy (DOE), the USGS collected 6,058 discrete hydraulic head measurements at various depths from 12 wells in the eastern Snake River Plain (ESRP) aquifer between 2007 and 2023. These measurements were derived from data on fluid pressure, fluid temperature, and atmospheric pressure. Each well was equipped with an MLMS, which included valved measurement ports, packer bladders, casing segments, and couplers. The MLMS allowed monitoring at 145 hydraulically-isolated depth intervals, reaching depths as great as 1,427 feet below the land surface. Additionally, 715 groundwater samples were collected from these wells between 2005 to 2023, and analyzed for a wide range of chemical and physical parameters."
   },
   {
     "pub_id": "TrckaOthers2024",