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Optimizing Sampling Strategies for Riverine Nitrate using High-Frequency Data in Agricultural Watersheds Kaycee N Reynolds, Terrance D. Loecke, Amy J. Burgin, Caroline A. Davis, Diego Riveros-Iregui, Steven A Thomas, Martin A. St.Clair, and Adam S. Ward Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.5b05423 • Publication Date (Web): 18 May 2016 Downloaded from http://pubs.acs.org on May 18, 2016

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Environmental Science & Technology

Optimizing Sampling Strategies for Riverine Nitrate using High-Frequency Data in Agricultural Watersheds

Kaycee N. Reynolds1, Terrance D. Loecke*1,2, Amy J. Burgin1,2, Caroline A. Davis3, Diego Riveros-Iregui4, Steven A. Thomas1, Martin A. St. Clair5, and Adam S. Ward6 1

School of Natural Resources, University of Nebraska-Lincoln, Lincoln, NE ([email protected], [email protected]) 2

Present address: Kansas Biological Survey and University of Kansas, Lawrence, KS ([email protected], [email protected]) 3

IIHR Hydroscience & Engineering, University of Iowa, Iowa City, IA ([email protected]) 4

Department of Geography, University of North Carolina, Chapel Hill, NC ([email protected])

5

Department of Chemistry, Coe College, Cedar Rapids, IA ([email protected])

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School of Public and Environmental Affairs, Indiana University, Bloomington, IN ([email protected]) Running Title: Sampling Frequency *Corresponding Author: Terrance D. Loecke Kansas Biological Survey University of Kansas 2101 Constant Ave. Lawrence KS, 66047 Date of Preparation: 21 March 2016, revisions post review for ES&T Revision/Version: 18 Word count: 4,600 (excludes references) # Figures: 4 # Tables: 2 # References: 47 In Review: Environmental Science & Technology Type of Contribution: Research Article Key Findings: 1) Fixed time-interval sampling has the greatest return on sampling investment by reducing uncertainty faster in estimates of mean nitrate concentration, proportion of yearly samples exceeding the nitrate drinking water standard, peak nitrate concentration, and nitrate flux compared to event-based strategies. 2) Storm sampling using a historical discharge threshold optimally characterized nitrate flux only at coarse frequencies. 3) Traditional sampling frequencies (i.e., bi-weekly and monthly) sufficiently characterize the four nitrate parameters considered in this study.

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ACS Paragon Plus Environment


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Abstract: Understanding linked hydrologic and biogeochemical processes such as nitrate loading

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to agricultural streams requires that the sampling bias and precision of monitoring strategies be

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known. An existing spatially distributed, high-frequency nitrate monitoring network covering

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~40% of Iowa (USA) provided direct observations of in situ nitrate concentrations at a temporal

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resolution of 15 minutes. Systematic subsampling of nitrate records allowed for quantification of

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uncertainties (bias and precision) associated with estimates of various nitrate parameters,

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including: mean nitrate concentration, proportion of samples exceeding the nitrate drinking water

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standard (DWS), peak (>90th quantile) nitrate concentration, and nitrate flux. We subsampled

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continuous records for 47 site-year combinations mimicking common, but labor intensive, water

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sampling regimes (e.g. time-interval, stage-triggered and dynamic-discharge storm sampling).

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Our results suggest that time-interval sampling most efficiently characterized all nitrate

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parameters, except at coarse frequencies for nitrate flux. Stage-triggered storm sampling most

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precisely captured nitrate flux when using less than 0.19% of possible 15-minute observations for

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a site-year. The time-interval strategy had the greatest return on sampling investment by most

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precisely and accurately quantifying nitrate parameters per sampling effort. These uncertainty

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estimates can aid in designing sampling strategies focused on nitrate monitoring in the tile-

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drained Midwest (USA), or similar agricultural regions.

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Keywords: High-frequency monitoring, Nitrate, water quality, error estimation, agriculture

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Introduction Agricultural practices accelerate nitrate leaching in cultivated landscapes,1 particularly in

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the Midwestern US where intensive agriculture and artificially-drained fields predominate.2–5

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Stream nitrate concentration variability can occur at timescales spanning minutes (episodic

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response), weeks (seasonal cycles) and decades (long-term trends) in response to dynamic

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hydrological processes.6,7 Variation in nitrate concentration associated with specific hydrologic

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events (e.g., storm events, climatic variability) can be a major source of sampling error when

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estimating nitrate flux.8 Inter-annual variation in nitrate flux from agricultural basins is primarily

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controlled by discharge (Q)9, with most nutrient losses occurring when discharge ≥ median Q,

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and more than 50% of export occurring during episodic precipitation events accompanied by

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extreme flow (>90th percentile Q).10,11 Generally, maximum storm-related nitrogen fluxes are one

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to two orders of magnitude higher than pre-storm fluxes.8 Thus, accurately capturing nitrate flux

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during extreme flow conditions is critical for reliable flux estimates.

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Despite the fact that sampling uncertainty is an inverse function of sampling frequency,

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logistical and budget constraints typically limit sampling efforts, which contributes to amplified

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errors in water quality parameter estimates.8,12,13 Water quality monitoring is often initiated to: 1)

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collect data for model development or validation, 2) verify effectiveness of best management

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practices, 3) measure water quality status for regulatory compliance, and 4) document existing

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background conditions to evaluate trends.12,14 Historically, water quality monitoring has relied on

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grab sampling at discrete time-intervals (e.g., bi-weekly or monthly) throughout the year, from

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which annual metrics are estimated.15 Although infrequent concentration measurements combined

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with mean daily stream Q may be acceptable for evaluating nitrate load on a seasonal or annual

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scale, such infrequent measurements may not sufficiently capture individual or sequenced event-

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related nitrate fluxes.6 More recently, monitoring agencies have invested in in situ sensors that

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measure nitrate concentrations at high-frequency intervals (e.g., seconds to minutes). These

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sensors provide nearly 3000 times more nitrate concentration data than monthly grab sampling. In

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Iowa, continuous nitrate sensing is used to manage drinking-water supplies and wastewater

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discharges as well as to track the effectiveness of agricultural best management practices.16

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Traditional labor-intensive sampling methods for estimating nutrient loads have cumulative uncertainties introduced by four procedural categories: stream flow measurement,

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sample collection, sample preservation/storage, and laboratory analysis.17 Of these, the strategy

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for collecting samples has the potential to introduce the most uncertainty, accounting for 4-48%

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of the error under typical collection scenarios.17 With limited monitoring resources, infrequent

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and cost-efficient sampling regimes will likely be the norm for the foreseeable future,18 thus

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making an assessment of the sampling uncertainty of simplified strategies critical.

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The use of spatially distributed, continuous real-time data presents an unparalleled

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opportunity to quantify uncertainties of conventional sampling strategies across a range of

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watersheds. We use such a database to ask: How is nitrate concentration and flux estimation

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uncertainty affected by sampling strategy? We address this question using a high-frequency

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nitrate monitoring dataset (n≈830,000) collected in watersheds covering 40% of the state of Iowa,

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the second largest agricultural producer in the United States.19 With more frequent sampling, we

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predicted that uncertainties associated with nitrate concentration and flux estimates would

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decrease. We expected the most frequent time-interval sampling strategy (i.e., daily) to provide

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the most precise estimates of mean nitrate concentration, proportion of yearly samples exceeding

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the nitrate DWS, peak nitrate concentration, and nitrate flux. Alternatively, we hypothesized that

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while the storm-based sampling regimes would likely increase uncertainty in mean nitrate

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concentration estimates, by targeting extreme Q, this regime is more likely to capture maximum

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concentrations and may be superior for characterizing the instances of stream water exceeding the

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nitrate DWS, peak nitrate concentrations and nitrate flux. Understanding how both timing and

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frequency of monitoring affects accuracy of nitrate parameter estimates will provide valuable

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insight for informed management and optimization of monitoring strategies in agricultural

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watersheds.

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Materials & Methods

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Catchment characteristics

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Nitrate (NO3--N) concentration and discharge (Q) were measured using in situ continuous

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monitoring sensors at 17 locations established by the USGS. Collectively, these 17 sites cover 11

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HUC-8 watersheds and drain 58,831 km2 (~40%) of Iowa (Figure SI-S1). Land used in these

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watersheds is predominantly agricultural, defined here as corn and soybean row crop (mean =

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72%; Table SI-S1), with growing urbanization in Des Moines, Cedar Rapids, and Iowa City. The

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watersheds used in our analyses were on average 45.5% corn, 26.2% soy and 15.8% other

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production.20 Iowa has a distinct four-season climate, with warm and humid summers, cool

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autumns, cold winters, and wet springs, reflective of the state’s mid-latitude and interior

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continental position.21 The annual average temperature ranges from 7.2-11.1°C and annual

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average precipitation ranges from 66-96.5 cm (from the NW to SE corners), with more than 75%

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of the annual precipitation falling during the growing season (i.e. April-September).22

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Due to poor soil drainage that causes fields to otherwise be submerged following storm

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events, agricultural fields are often outfitted with underground tiles that drain water quickly from

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the soil-rooting zone.23 The extent of artificial drainage is difficult to estimate, but conservatively

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covers 32% of Iowa cropland.24 The presence of drainage tiles rapidly connects the land surface,

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vadose zone, and shallow groundwater to the stream network. Tile drainage allows for the rapid

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transport of nitrate, originating from agricultural practices, into nearby surface waters; a system

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that results in high nitrate concentrations in Iowa streams.25,26 Nitrate yields from Iowa rivers are

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some of the highest in the nation,2 often ranking the state near the highest in terms of estimated

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total flux of nitrogen contributed to the Gulf of Mexico Hypoxic “Dead Zone”.27

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High-frequency monitoring sensors

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As of 2013, the United States Geological Survey (USGS) and partner organizations

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monitored nitrate continuously at 44 locations in the continental USA;28 17 of these locations

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were used in this study (Table SI-S1). The USGS measures Q and in situ stream nitrate

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concentration at a 15-minute interval. Stream nitrate is recorded as nitrate+nitrite as N (mg NO3--

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N L-1) using a Hach Nitratax plus sc Sensor (2 mm path length; Loveland, CO, USA), which has

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a measurement range of 0.1-50 mg NO3--N L-1 and a 0.1 mg NO3--N L-1 resolution (measuring

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error: ±3% of the mean MW± 0.5). Gaps in the datasets reflect operational issues with the

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equipment or periods when the sensor was retrieved for calibration and servicing. Most of the in

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situ sensors operate from early spring (mid-March to mid-April) through early winter (mid-

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November to mid-December) when data collection is suspended because the sensors cannot

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function below 2°C.29 Stream Q was estimated using site-specific rating curves based on

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continuously recorded gage height and discretely measured streamflow.30 Long-term Q data were

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obtained from the USGS National Water Information System.31

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Nitrate Parameters

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We analyzed results for four nitrate parameters: mean nitrate concentration (CM),

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proportion of observations exceeding the 10 mg NO3--N L-1 EPA Maximum Contaminant Level

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(MCL) for nitrate, (MCLP),32 peak (>90th quantile) nitrate concentrations (CP), and nitrate flux

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(FT). Each parameter was evaluated over the range of dates included in each site-year. Mean

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nitrate concentration (CM) was calculated for each of the 47 site-years as =

Σ()

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where C(t) represents the 15-minute nitrate concentration readings and n is the number of

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concentration observations for a site-year based on calendar years. The MCLP, often referred to as

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the nitrate DWS, was determined for each site year using the empirical cumulative distribution

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function in R.33 The 90th percentile of the nitrate concentration for each site year (CP) was

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determined using R. Instantaneous nitrate mass flux is the product of Q and concentration at each

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time step. Nitrate mass flux (FT), often referred to as load, over a period of interest from 0 to T,

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can be calculated by integration as

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= () ()d

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where, 0 and T are the earliest and latest sample date/times, respectively, for a site-year.

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Estimation of nitrate flux is typically based on available data, which often consists of frequent Q

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(e.g. often mean daily Q) and infrequent concentration.34 The advent of high-temporal resolution

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sensors for measuring in-stream nitrate concentrations enables us to calculate these quantities at

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much higher temporal resolution than heretofore possible and reduce error introduced by

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averaging.

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Sampling regimes

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Three separate sampling regimes were tested here: time-interval, stage-triggered storm

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sampling, and dynamic-Q storm sampling (Figure 1). Time-interval sampling mimics manual

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grab sampling at four time-intervals: daily (Figure 1A), weekly, bi-weekly and monthly.

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Sampling was limited to weekdays (i.e. Monday-Friday) and typical working hours (09:00-

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17:00). Storm sampling mimics the use of a programmed auto-sampler triggered based on Q, [e.g.

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Teledyne ISCO (Lincoln, NE, USA)]. Both stage-triggered and dynamic-Q storm sampling

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randomly drew from a storm-hydrograph at four frequencies: once during an event, twice during

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an event, daily during an event (Figure 1B-C) and hourly during an event. In addition, two

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stratified sampling frequencies: monthly + hourly during an event, and weekly + hourly during an

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event were considered, combining time-interval and storm sampling strategies. All sampling

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strategies were applied to each of the 47 site-year combinations. For each strategy we drew

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random samples from the continuous dataset, which included the timestamp and associated nitrate

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concentration, Q, and instantaneous flux. Sampling effort, defined as the proportion of samples

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used for each sampling frequency, was calculated as the number of sample draws from the total

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number of 15-minute samples available for a site-year. Using systematic and Monte Carlo

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sampling, we generated sample subsets from the continuously collected nitrate data using

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predetermined, common sampling strategies. As the number of sample iterations increases, the

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variability will decrease until it reaches a point where we can assume it is representative of the

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population.35 Based on previous simulations in the literature,35,36 500-interations was deemed

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sufficient for this study. Subsampling was conducted with replacement.

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Unique storm events for each site-year dataset were labeled based on stage-triggered and

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dynamic-Q thresholds. The stage-triggered approach set the storm threshold as the 90th percentile

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of the historical (all possible years 1907-2013) Q data for each site (Figure 1B). Extreme

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discharges (>90th percentile) contribute >50% of the nitrate export in the Midwest.11 The start of a

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unique event was signaled when this Q threshold was surpassed for two consecutive readings

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(i.e., ~30 min) and ended when Q fell below this threshold for two consecutive readings (Figure

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1B). For the dynamic-Q threshold approach, we calculated the distribution of percent change in Q

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over two hour intervals for each site-year. The 99th percentile of this distribution was used as the

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dynamic-Q threshold for that site-year. The 99th percentile was chosen to capture a similar

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number of events as the stage-triggered threshold. This more flexible threshold allowed us to

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sample both small and large storm events within each site-year. A unique event began when the

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percent change in Q exceeded this threshold (Figure 1C) and ended when Q returned to its start

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value for that event or, in instances where Q does not return to its start value, one time point

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before the next event was initiated (Figure 1C). Only events longer than 48 sampling periods (i.e.,

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½ a day) were included; events were also limited to a 5-day duration maximum. Once unique

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events were labeled for each site-year based on the two separate thresholds, storm sampling at

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each of the aforementioned frequencies was carried out to simulate sampling either by manual

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storm-chasing (i.e., sampling once or twice during an event) or by an automatic Q-induced

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instrument sampling daily or hourly during an event.

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Using the subsampled time series, nitrate concentration was linearly interpolated between

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the sampled points (i.e., daily, weekly, monthly) for each 15-minute time step from the first draw

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(minimum Date/Time) for that site-year to the last draw (maximum Date/Time). This was paired

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with the corresponding 15-minute Q value collected at the same date/time for that same site-year.

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By integrating the instantaneous flux over the time period from initial to final sample for that site-

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year, we were able to calculate nitrate flux as:

= () ()d

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where C0 is instantaneous nitrate concentration, Q0 is the paired instantaneous discharge, and 0

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and T are the earliest and latest date/time for that sample iteration. These calculated subsample

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nitrate fluxes were compared to the nitrate flux for that site-year, calculated from the continuous

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nitrate concentration and Q data.

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Quantifying Sampling Uncertainty

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For each sampling strategy-frequency combination (i.e., sampling regime) and nitrate parameter, the sampling bias was quantified relative to the parameter mean as follows: ! =

"# × 100 $̅

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where ME is the mean error (i.e., deviation) between the calculated nitrate parameter from each

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subsample (n=500) and that calculated from the 15-minute complete sensor data set, $̅ is the

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calculated nitrate parameter from the complete data set of that particular site-year combination.

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Relative bias is expressed as a percentage.

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For each sampling strategy-frequency combination (i.e., sampling regime) and nitrate parameter, the sampling precision was quantified as the coefficient of variation (CV) as follows: ) =

"*# × 100 $̅

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where RMSE is the root mean squared error (i.e., deviation) between the calculated water

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parameter from each subsample (n=500) and that calculated from the 15-minute complete sensor

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data set, $̅ is the calculated nitrate parameter from the complete data set of that particular site-

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year combination, and CV is expressed as a percentage.

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Statistical Analysis and Model Development

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Kruskal-Wallis multiple comparison tests were used to determine time-interval sampling

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effects on sampling precision for each of the four nitrate parameters.37 A linear mixed effects

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analysis of the relationship between natural log of CV and sampling effort was conducted using

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the lme4 package in R.38 We included sampling effort (i.e. proportion of possible samples) and

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sampling type (with an interaction term) as fixed effects. The random effects in the model were

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an intercept for site-year, as well as by-site-year random slopes to control for inherent differences

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among sites and years. The response, CV(%), was natural log-transformed to reduce

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heteroskedasticity and to meet the assumption that residuals in the model have similar deviations

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from predicted values.

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Results Near continuous monitoring of 17 Iowa streams yielded 829,968 instantaneous in situ

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nitrate concentration measurements and 1,158,100 Q estimates. Mean nitrate concentrations

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ranged from 1.5 (±0.4) to 32.5 (±6.7) mg NO3--N L-1 (±1 standard deviation) and mean Q ranged

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from 0.5 (±0.9) to 376.9 (±361) m3 s-1 (Table SI-S2). Across the 47 site-years, the highest

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monthly mean nitrate concentrations were observed in May (11.8±6.5 mg NO3--N L-1) and June

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(10.7±5.7 mg NO3--N L-1), while the highest mean Q was observed in June (156±296 m3 s-1) and

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March (140±275 m3 s-1) (Table SI-S3). The mean nitrate concentration across all sites was highest

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in 2008 (9.3 mg NO3--N L-1) and had the largest range in 2013 (±7.9 mg NO3--N L-1), while Q

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was highest on average and most variable in 2010 (195±282 m3 s-1; Table SI-S4 and SI-S5). The

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nitrate drinking water standard (DWS; 10 mg NO3--N L-1) was exceeded in 37 of the 47 site-

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years. Six of the 10 site-years that did not exceed the DWS occurred during 2012, the driest year.

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Across all sites, instantaneous nitrate concentration was most variable from May-July, while

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instantaneous Q was most variable during March, May and June (Table SI-S3). Peaks in

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discharge occur most frequently May and June, which corresponds to the highest average rainfall

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of all months (12.1 and 13.0 cm respectively).39

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Sampling bias and precision vary with monitoring strategy and parameter of interest

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(Figures 2 and 3). Time-interval sampling decreased bias and increased precision for

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characterizing nitrate concentration more than either stage triggered or dynamic-Q threshold

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strategies (Figure 2A-B and Figure 3A-B). This lack of systematic bias indicates sampling during

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“normal work hours” sufficiently characterizes diurnal nitrate concentration patterns across these

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watersheds. Within the time-interval strategy, precision improves on average 11 to 14-fold

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among nitrate concentration parameters as sampling frequency increases (i.e., from 9.7%-0.9%

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for monthly to daily frequencies when estimating mean nitrate concentration; Figure 3A). The

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precision of daily sampling averages 0.9% of the parameter mean for mean nitrate concentration,

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0.9% for the proportion of samples exceeding the nitrate DWS, and 0.9% for the peak nitrate

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concentration estimates (Table 1). For all frequencies in this strategy, even traditional monthly

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sampling, median CV for nitrate concentration parameters were 1.3% of total possible

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samples, in which case, it actually amplified uncertainty making dynamic-Q the more

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advantageous storm sampling approach (Figure 4C). Additionally, when using > 0.2% of possible

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samples the time-interval strategy was more precise for flux estimates than stage-trigged storm

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sampling (first crossover point; Figure 4D).

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Discussion

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Optimizing monitoring strategies by nitrate parameter

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Optimal sampling strategy is a function of the parameter of interest, the costs associated

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with equipment and person-power, and the ultimate objective of the monitoring. The time-interval

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strategy was the best monitoring strategy to improve precision without sacrificing accuracy (i.e.,

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systematic bias) in mean nitrate concentration, proportion of samples exceeding the nitrate DWS,

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and peak nitrate concentration (Figures 4A-C). However, optimization for nitrate flux was

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dependent on the sampling effort (Figure 4D). When sampling < 0.2% of the total possible 15-

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minute samples at a site, stage-triggered storm sampling was optimal; when sampling more

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frequently, the time-interval strategy quickly became optimal. For our 47 site-years, this meant

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stage-triggered storm sampling was optimal at coarse frequencies (1-2 samples per event), while

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the time-interval strategy optimally characterized nitrate flux at weekly to daily frequencies

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(Figures 4D and SI-S2). Dynamic-Q storm sampling was the least optimal strategy for any of the

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nitrate parameters. Thus, if characterizing nitrate concentration parameters is the primary interest,

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as is often the case for understanding water quality entering a municipal water supply, a time-

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interval based strategy is the best investment of monitoring resources. However, if the monitoring

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goal is to understand fluxes of nitrate heading towards connected downstream waters, as is the

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case for efforts to reduce nutrient loading to coastal areas including the Gulf of Mexico, stage-

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triggered sampling is best given infrequent sampling, but can quickly be outpaced by time-

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interval strategies.

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Estimating sampling bias and precision allows for optimization of monitoring

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methodologies, improvement in decision-making and regulatory development, and contributes to

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model calibration, validation and ultimately application.40 Quality assurance protocols are

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implemented by water monitoring agencies to reduce overall uncertainty; however, sampling bias

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and precision estimations were previously under-quantified or overlooked due to lack of high-

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frequency data with which to compare sample estimates. Many previous studies have noted the

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substantial errors in water quality parameter estimates that result from infrequent sampling;

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however, most lacked continuous data sets with which to compare parameters estimated from

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infrequent sampling.34,41–44 For example, Alewell et al.41 aimed to understand if the gain of

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information with ‘high resolution’ daily measurements outweighed the additional efforts and

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associated costs compared to weekly or bi-weekly sampling. Their results indicated that bi-

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weekly sampling accurately characterized ion fluxes in a semi-natural ecosystem and that any

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additional information gained by daily sampling was not worth the additional effort. However,

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they noted the dynamic nature of agricultural systems and conceded that these conclusions may

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not hold in agricultural landscapes. Our results indicate sampling precision is significantly

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improved when going from bi-weekly or weekly to daily sampling for all four nitrate parameters;

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however, there is no significant difference in sampling precision or bias between bi-weekly and

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weekly sampling. Therefore bi-weekly sampling is recommended for mean and peak nitrate

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concentrations in this system, as it sufficiently characterized these nitrate parameters, contributing

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on average 3.6% and 4.9% margin of precision to estimates across all 47 site-years (Table 1).

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There was no significant difference in sampling precision induced by bi-weekly vs. monthly

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sampling for the proportion of samples exceeding the nitrate DWS or nitrate flux, so the coarser

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frequency, monthly, could be a reasonable approach to reduce costs.

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Combining data-driven monitoring optimization with non-data sampling limitations

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Our results indicate that daily time-interval sampling resulted in the best sampling

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precision for all nitrate concentration related parameter estimates, while the most frequent stage-

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triggered storm sampling frequency resulted in the best sampling precision in nitrate flux

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estimates. Although these strategies provided the most precise and accurate estimates, they may

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not be economically feasible long-term or across a large spatial extent. Understanding the

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marginal return on sampling effort allows us to obtain more useful information and adjust

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sampling strategy or frequency to balance effort and accuracy. Based on our results, traditional

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sampling frequencies (i.e., bi-weekly and monthly) would characterize mean nitrate

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concentration, the proportion of samples exceeding the DWS, peak nitrate concentrations and

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nitrate flux, without bias with a precision of 90th quantile), and (D) flux as a function of sample proportion. The proportion of possible samples used represents sampling intensity; as you go from left to right across the x-axis, sampling gets more frequent.

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List of Tables

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Table 1. Median precision for all sampling regimes across 47 site-years. Each row represents a sampling strategy-frequency combination. The columns show the median precision induced by a particular regime as the coefficient of variation with Q1 and Q3 in parentheses to indicate spread. Sampling Regime

Sampling Frequency

Time-Interval

Daily

Time-Interval

Weekly

Time-Interval

Bi-Weekly

Time-Interval

Monthly

Stage-Triggered Storm Stage-Triggered Storm Stage-Triggered Storm Stage-Triggered Storm Stage-Triggered Storm Stage-Triggered Storm Dynamic-Q Storm Dynamic-Q Storm Dynamic-Q Storm Dynamic-Q Storm Dynamic-Q Storm Dynamic-Q Storm

Weekly + Hourly/event Monthly + Hourly/event Hourly/event Daily/event 2x/event 1x/event Weekly + Hourly/event Monthly + Hourly/event Hourly/event Daily/event 2x/event 1x/event

Median CV for CM (Q1-Q3) 0.9 (0.4-1.9) 2.6 (1.8-5.9) 3.6 (2.7-6.5) 9.7 (7.4-14.2) 51.6 (19.1-90.5) 53.1 (19.3-96.1) 53.6 (20.4-96.8) 51.23 (20.3-96.4) 49.7 (18.2-84.2) 49.6 (18.7-84.7) 20.2 (8.2-39.6) 21.4 (9.4-41.5) 21.8 (9.6-42.5) 20.1 (8.5-35.6) 17.1 (8.4-33.2) 18.0 (9.4-33.8)

Median CV for MCLP (Q1-Q3) 0.9 (0.8-1.7) 3.9 (2.3-6.2) 5.7 (4.0-9.7) 13.3 (8.2-17.9) 58.6 (21.4-79.8) 66.7 (21.7-88.5) 69.4 (21.8-96.1) 60.7 (21.1-94.4) 65.7 (21.3-96.7) 66.8 (23.6-96.6) 16.1 (5.9-33.7) 16.7 (6.1-35.3) 17.1 (6.2-36.0) 13.0 (5.1-31.1) 12.7 (5.7-30.6) 14.0 (7.7-31.6)

675 676 677

28


Median CV for CP (Q1-Q3) 0.9 (0.5-1.9) 3.6 (2.2-6.0) 4.9 (3.0-6.7) 12.4 (7.7-15.9) 10.0 (5.5-18.8) 10.1 (5.6-19.0) 10.1 (5.6-19.1) 9.6 (4.8-17.2) 8.8 (4.7-16.8) 7.1 (5.4-16.5) 12.5 (4.5-4.7) 12.8 (4.9-26.5) 12.9 (5.0-27.7) 10.8 (5.5-26.5) 12.3 (6.7-25.7) 13.1 (7.4-22.9)

Median CV for FT (Q1-Q3) 1.1 (0.5-2.0) 3.2 (2.5-5.6) 5.4 (3.7-9.5) 9.9 (7.7-15.5) 0.7 (0.4-1.5) 1.7 (1.0-3.5) 1.5 (0.3-3.6) 2.2 (1.0-4.8) 8.1 (5.2-10.8) 10.3 (6.5-13.7) 1.8 (1.3-3.1) 3.9 (2.6-7.1) 5.8 (2.1-13.2) 9.2 (4.3-16.3) 11.1 (7.3-16.6) 12.3 (8.3-19.7)

Page 29 of 29

678 679 680 681 682 683


Table 2. Linear mixed-model intercepts and slopes for each sampling strategy. Each row represents a sampling strategy: Time-Interval (TI), Stage-Triggered Storm Sampling (ST), and Dynamic-Q Storm Sampling (DQ. The columns show the intercepts and slopes with standard error for each of the mixed-models in Figure 3. Note: *Slope not significantly different from 0 (t value0.05), aNot significantly different from one another, +Not highly significant (p-value

Optimizing Sampling Strategies for Riverine Nitrate ... - ACS Publications

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