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Article

Holistic Approach for Estimating Water Quality Ecosystem Services of Danube Floodplains: Field Measures, Remote Sensing, and Machine Learning

Chair of Hydrology and River Basin Management, TUM School of Engineering and Design, Technical University of Munich, Augustenstraße 44, 80333 Munich, Germany
*
Author to whom correspondence should be addressed.
Hydrobiology 2022, 1(2), 211-231; https://doi.org/10.3390/hydrobiology1020016
Received: 31 March 2022 / Revised: 10 May 2022 / Accepted: 11 May 2022 / Published: 16 May 2022

Abstract

:
Human pressure has caused river ecosystems to be severely damaged. To improve river ecosystems, “working with nature”, i.e., nature-based Solutions (NbS), should be supported. The purpose of this paper is to evaluate the effects of a specific NbS, i.e., floodplain restoration, which provides, among others, the ecosystem service of nutrient retention. For these, an in-depth time series analysis of different nutrients’ concentrations and water physiochemical parameters was performed to obtain Water Quality Indices (WQI), which were calculated along the river. To estimate water quality from remote sensing data and to generate water quality maps along the river, Sentinel-2 water products were validated against in situ data, and linear regression (LR), random forest (RF), and support vector regression (SVR) were trained with atmospherically corrected data for chlorophyll-a and TSM. The results show different outcomes in diverse floodplains in terms of improvement of the water quality downstream of the floodplains. RF demonstrated higher performance to model Chl-a, and LR demonstrated higher performance to model TSM. Based on this, we provide an insightful discussion about the benefits of NbS. These methodologies contribute to the evaluation of already existing NbS on the Danube River based on a quantitative analysis of the effects of floodplain ecosystems to water quality.

1. Introduction

1.1. Research Context

Nature-based solutions (NbS) are “actions which are inspired by, supported by or copied from nature”, that are potentially “energy and resource-efficient and resilient to change” [1]. NbS can solve water management problems, restore ecosystems, and increase sustainability [1,2,3]. An ecosystem is at the center of the NbS implementation areas.
Human pressures have caused river ecosystems to be seriously damaged in the entire world. Over the past 50 years, pollution, nutrient enrichments, dam constructions, and unsustainable exploitations have led to rivers’ deterioration. For example, the interruption of migratory routes of fish species by dam and weir constructions has led to a critical decrease of these fish species or even for their extinction [4]. One major cause of river ecosystems’ degradation is nutrient pollution. It is causing growth of dangerous algal blooms in new river locations, where they have different toxicity levels, and they are lasting for longer hours [5]. Agricultural practices, river modifications, bank erosions, and fertilizer applications have caused a huge increase in nutrient loads in rivers, mainly from nitrogen (N) and phosphorus (P) [5,6,7,8,9]. Nitrogen is present in waterways by the forms of nitrite (NO2), nitrate (NO3), ammonium (NH4+), and organic N; phosphorus is present as particulate P, and soluble reactive P (SRP).
A good example for an NbS dealing with the degradation of river ecosystems is floodplain restoration. Floodplains are a space alongside a watercourse, which are typically developed by deposition of solid particles in the course of floods of different magnitude [10,11], where water, nutrient, sediment, and organism exchanges are happening [12,13]. Flooding events, ranging from frequent and very low discharge events to less frequent and high discharge events, support the dynamics of the floodplain ecosystem and impact multiple biophysical features (e.g., hydro-morphological features and soil hydrology). Additionally, floodplains play an important role for the natural functioning of a river [14,15], and provide ecosystem functions and ecosystem services (ES), i.e., “the quantifiable or qualitative benefits of ecosystem functioning to the overall environment, including the products, services, and other benefits humans receive from natural, regulated, or otherwise perturbed ecosystems” [16]. One of the most important ES of floodplains is the transformation and retention of nutrients in river streams [17,18,19], identified by nitrate-N, total particulate P, the Water Quality Index (WQI), or concentrations of chlorophyll-a (Chl-a) and total suspended matter (TSM).

1.2. Background

Nitrate-N and total particulate P are the two primary forms of N and P in floodplain studies [20], and are retained by denitrification for N [21] and sedimentation for P [22].
WQI is generally used to assess the quality of both groundwater and surface water (e.g., rivers), and it is very important to compute when dealing with water resources management [23,24,25]. WQI consists of combining multiple natural parameters (e.g., nutrients in water concentration and water physiochemical parameters), and translate them efficiently into a single value, reflecting the quality of water.
Satellite remote sensing is an approach to retrieve water quality parameters such as Chl-a and TSM [26], which according to the Water Framework Directive (2000/60/EC) (WFD), are very important to monitor, since they are one of the lead parameters that described the trophic state of water, in addition to phytoplankton biomass [27,28,29] and water clarity [30]. One example of a satellite remote sensing tool is the MultiSpectral Instrument (MSI) onboard Sentinel-2 (S2), which has a high resolution of up to 10 m, and it has shown very good results in estimating the Chl-a and TSM concentrations in lakes [31]. For complex waterbodies, additional studies for atmospheric correction (AC) algorithms can be developed [32]. For this reason, the Copernicus Program developed an open source database for satellite imagery to improve monitoring [33] through modeling. In fact, modeling can be used to set up a relation between the radiometric values obtained from satellite images and the in situ measurements acquired in a matching date. These relationships can be sorted as empirical, semi-analytical, or based on machine learning (ML) [34], e.g., through multivariate linear regression (MLR), random forest (RF), support vector regression (SVR), or neuronal networks models. ML is considered a novel field of study, hence it is still not very efficient in water quality estimation, and it is very important to understand its behavior in remote sensing for a better estimation of inland water qualities [35].

1.3. Research Objective

To understand the effects of nutrient retention in potential floodplain restoration NbS, we investigated the situation of water quality along the Danube River in time and space, and analyzed the effects of already existing, i.e., active, floodplains. Estimating the actual effect of floodplains on the retention of nutrients is a laborious process, which requires a high amount of measured data and/or proper modeling. Therefore, with this study, we aim at observing nutrient retention on the Danube, by analyzing nitrate-N, total particulate P, WQI, Chl-a, and TSM, and estimating their changes along the Danube floodplains.
To reach this main goal, different sub-objectives were set:
  • displaying the behavior of specific parameters with a temporal analysis of water quality with field data from 1996 to 2017;
  • investigating particular changes of the water quality at the spatial level through all active floodplains along the Danube River;
  • assessing the effect of floodplains’ nutrient retention and water quality improvement by means of time series analysis of nutrients, physiochemical parameters, and WQI;
  • analyzing the relationship between the river discharge and river water quality through correlation analysis between the nutrients’ retention values and the river discharge, as well as between the water quality improvement and the river discharge.
Moreover, remote sensing-based ML models (MLR, RF, and SVR) were trained using field measurements and Sentinel-2 products, to investigate the situation of water quality using satellite imagery and to generate water quality maps, describing the situation of water quality through all active floodplains along the Danube River.
The Danube River was chosen in our study because nearly all the floodplains of the large rivers located in Central Europe (e.g., the Rhine, Elbe, Danube, and Oder) have suffered degradation due to agricultural activities, structural flood protection measures, dam constructions, and land-use changes (urbanization and transport infrastructure) [36,37,38,39].

2. Study Area

We investigated floodplains located along the Danube River (Table 1). The river originates in West Germany and its outlet is in the Black Sea. In total, 17 active floodplains within the Danube River Basin were selected as targets. These were derived within the Danube Floodplain Project (Figure 1), which defined active floodplains as inundated areas (hydraulically active) during a flood event with a return period of 100 years (HQ100), and identified them through a ratio factor between the widths of floodplain and river, a minimum threshold to the size, and hydraulic characteristics of the floodplain (e.g., flow paths, stages, and natural flow characteristics should be maintained) [40].
This area is relevant since the Danube has lost 80% of its former floodplains due to anthropogenic influence [41]. To monitor water quality dynamics in the river, field data measurements were acquired from multiple stations located in the vicinity of each floodplain. To analyze changes in water quality before and after each floodplain, we classified these stations as “upstream” and “downstream”. The restoration demand of each floodplain was reported as estimated from the Danube Floodplain Project (https://www.interreg-danube.eu/approved-projects/danube-floodplain (accessed on 10 December 2021) [42], indicating the level of restoration needed of each floodplain to regain its maximum functionality (e.g., providing groundwater recharge, filtering contaminants, supporting habitats, or transporting nutrients) (Table 1).

3. Materials and Methods

3.1. Evolution of Water Quality in the Danube River

3.1.1. Field Data

Information on the active floodplains and their restoration demand were retrieved from the open-source GIS website (http://www.geo.u-szeged.hu/dfgis/ (accessed on 10 December 2021) which provides spatial results of the Danube Floodplain Project [43]. Field data were retrieved from the Danube River Basin Water Quality Database [44]. Field measurements of hydrological variables are provided together with concentrations of different nutrients and other water physiochemical parameters. The water parameters used are river discharge, concentrations of ammonium, chlorophyll-a, nitrates, total nitrogen, and total phosphorus, in addition to conductivity, dissolved oxygen, pH, and total suspended matter.

3.1.2. Time Series Analysis

To understand the evolution of water parameters, time series graphs for each active floodplain (upstream and downstream) were analyzed. The values were aggregated to monthly and yearly averages, and important flood events were highlighted in the respective time frame to better understand the influence of these extreme events on the respective floodplains [44]. Complete time series plots for all floodplains and water parameters are provided in Figures S1–S10. Time series values were used to compute the nutrient retention, calculate the WQI, and compute the water quality improvements between upstream and downstream locations in relation to each active floodplain of the Danube River.

3.1.3. Floodplains and Data Availability

Based on data availability for each floodplain, nutrient retention and WQI were computed. Among all the floodplains analyzed (Table 1), we calculated the nutrient retention for both nitrogen and phosphorus for floodplains FP1, FP2, FP3, FP9, and FP10. As for the WQI, this was calculated for floodplains FP2, FP3, FP6, FP7, FP8, FP9, and FP10.

3.1.4. Nutrient Retention

The evaluation of water quality can be achieved by monitoring nutrient concentrations, and especially the nutrients that can provide information on the river’s trophic status, such as nitrogen (N) and phosphorus (P). To evaluate the contribution of a river, or in our case, a floodplain, to the nutrient balance of a system, nutrient loads and improvement or deterioration of water quality should be monitored [45]. However, there are no methods to measure nutrient loads directly [46]. Computing in-stream nutrient loads depends on the availability of data for the corresponding nutrients, and it can be done by different calculation methods. In general, they are the product of the nutrient concentration and the river discharge value [46]. Nutrient retention in floodplains can be then calculated by subtracting the nutrient load exiting the floodplain from the nutrient load entering it. Still, uncertainties in computation must be considered, since previous studies showed that nutrient loads computed from continuous river discharges and monthly nutrient concentrations (as in our case) deviate by 25% from the true values [47]. These deviations are caused by missing nutrient concentration peaks due to low frequency measurements (one time per month) and can lead to under- or over-estimation [47].
In our study, we computed the nitrate-N retention, as it is the primary form of nitrogen [20] and the total phosphorus retention in the different active floodplains of the Danube River, using the values generated from the time series analysis. Generally, nutrient retention in floodplains is computed per unit area of floodplain. For this study, the major interest was in the effects of nutrient retention in the active floodplains along the Danube River and not in retention rate per unit area. Therefore, only retentions in terms of nutrient loads were computed.

3.1.5. Water Quality Index (WQI)

WQI is a simple and efficient method to monitor the quality status. To describe the effect of floodplains in river restoration, we calculated the WQI upstream and downstream of each floodplain, and the WQI improvement in each floodplain. The WQI was calculated using Equation (1), developed to assess river water quality by Rodriguez de Bascarán [48,49], and the water parameters generated as described in Section 3.1.2.:
WQI = C i W i W i ,
where Ci represents a normalized assigned value (in percent) for each parameter value and Wi represents a weight for each parameter, ranging from 1 to 4, where 1 represents a minor importance for the ecological life and 3 represents a major importance.
Two of the parameters used in the calculation of the WQI developed by Rodriguez de Bascarán [48,49] are the Chemical Oxygen Demand (COD) and the Total Dissolved Solids (TDS). Since COD and TDS are not available in our dataset, COD was replaced by Chl-a because a significant positive correlation was shown between COD and Chl-a [50]. Additionally, TDS was replaced by TSM, since it is the only parameter describing the hardness quality of water in our data [30]. This decision was supported by previous studies where TSM was used in the calculation of the WQI [51,52].

3.1.6. Correlation with River Discharge

An active floodplain is a hydraulically active area inundated by flood event with return period of 100 years [44]. Since the aim of this study is to understand the nutrient retention effect in active floodplains, it was important to focus on the river discharge values leading to a floodplain being active. For this matter, a correlation analysis was conducted between the nutrient retention in floodplains and the river discharge values, in addition to another correlation analysis between the water quality improvement values (using the WQI improvement values) and the river discharge values. The analysis was done by calculating the Pearson’s correlation coefficient. This analysis was used to determine the relationship between the discharge values and the water quality.

3.2. Modeling Water Quality Dynamics with Remote Sensing

Different products available from remote sensing sensors can be used to monitor water quality parameters. We focused on Chl-a and TSM, and analyzed their concentrations. These two variables, considered important indicators for water environmental quality evaluation [53,54], can be monitored by remote sensing sensors since they are considered optically active components [55], and ready-to-use products are available from atmospherically corrected procedures. There are several studies showing that the capabilities of Sentinel-2 products are suitable to estimate Chl-a and TSM in water [31,54,55,56], but with some challenges in retrieving accurate data [32]. Sentinel-2 temporal (5 days) and spatial (10 m) resolutions contribute to consider this satellite as one the few suited to analyze a narrow water body as a river, but still wide enough as the Danube River. To evaluate the usefulness of available remote sensing products, we compared remotely derived Chl-a and TSM against field-measured parameters. To further model water quality changes in the river surface, atmospherically corrected remote sensing reflectance and several spectral-derived features were used as input features to supply ML algorithms, and produce further spatial and temporal analyses.

3.2.1. Field and Remote Sensing Data Comparison

The field measurement data for the Chl-a and TSM concentrations were retrieved from the Danube River Basin Water Quality Database by the International Commission for the Protection of the Danube River (ICPDR) [44]. The Copernicus Open Access Hub (https://scihub.copernicus.eu/ (accessed on 16 December 2021) was used to download cloud free Sentinel-2 S2 MSI Level-1C (L1C) data for the period 2014–2017 over the area of interest. An allowed period of a ±3 day difference between the S2 image and its corresponding in situ measurement was taken into consideration while matching up data [34]. Then, the images were processed using SNAP (v8.0.0.0), the open access toolbox for processing Sentinel missions. A standard atmospheric correction was applied to account for the scattered signal of the atmosphere, and retrieve remote sensing reflectance (RRS) to further modeling process [55,57]. The Level 1C data from Sentinel-2 was processed using the Case 2 Regional Coast Color (C2RCC) algorithm [57], which uses a large database of Chl-a and TSM concentrations trained with neural network, as well as using extreme ranges of scattering and absorption properties. The C2RCC processor is adequate for optically complex Case 2 waters (as the Danube River) which also retrieves layers of Chl-a and TSM concentrations [58]. These products are evaluated against available in situ data using conventional error metrics, such as the coefficient of determination (R2) and the Root Mean Squared Error (RSME).

3.2.2. Machine Learning Models

After C2RCC product validation, modeling was conducted by means of three ML algorithms, which were assembled and trained to estimate the Chl-a and TSM as targets. The input features were the remote sensing reflectance bands from C2RCC and further derived radio spectral features. MLR [59,60,61,62,63], RF [64,65,66], and the SVR [67,68,69] were considered since they are becoming standard algorithms in ML modeling of water quality [64]. All ML algorithms were implemented in Python 3.10.0 using the Scikit-Learn 1.0.2 library. Feature engineering was used to develop additional predictors to test more modeling scenarios [34,70,71,72]. The complete additional feature combinations were also tested in related research of remote sensing of inland waters [72].
To select the most adequate predictors, all the predictors were tested with the Pearson’s correlation against Chl-a and TSM. The highest correlated features were then selected as input for the algorithms. To tune algorithm hyperparameters, we used a Grid Search with predefined values. The final dataset of remote sensing reflectance and target parameters was divided into train and test splits and evaluated using a leave one out cross-validation (LOOCV) [35]. LOOCV is a specific case of a K-fold cross-validation where K equals N (the number of data points), which eliminates biases that a single split in the dataset may cause by using this technique. This method partitioned the dataset into K-fold of freely selected observations. Every model was trained for each of the K possible training-test splits, and the reported values for R2 and RMSE were the average of these K runs.
Finally, the model with the best error metrics values was chosen for estimating Chl-a and TSM over the surface of the Danube River to visualize spatial distributions based on specific dates and locations detected in the time series and WQI variations on each floodplain. The complete process which summarizes the methodology applied in this work is shown in Figure 2.

4. Results

4.1. Results on Water Quality Index (WQI)

Results indicate, in general, that floodplains act positively by improving water quality in floodplains (Figure 3). We can notice an improvement in water quality between upstream and downstream for the majority of years in FP2, FP6, FP7, FP8, and FP9. Floodplain FP3 also shows an improvement in water quality for some years, however, it displays very little data. Floodplain FP10 acts quite the opposite to the other floodplains, as it does not show any improvement of water quality downstream of the floodplain in any year.
The percentage of improvement of WQI is still conservative and is usually below 8% for the whole period of analysis, with exception to FP8, which shows improvements of up to 20% (in 2015). Similarly, a decrease in WQI reaches maximum 7% for all floodplains except for FP10, which displayed WQI reductions up to 11%.

4.2. Nitrogen and Phosphorus Retention

Average yearly retention values for nitrates and phosphorus are shown in Figure 4. It can be seen that both FP2 and FP10 retain nutrients, whereas neither FP3 nor FP9 promote retention. On the other hand, FP1 retains very small amounts of nitrate but does not fortify phosphorus retention in cases when the retention load is too large.

4.3. Water Quality Variations

By averaging the improvement and worsening results of WQI, it is possible to have an overall view of the water quality variations. Results of this exercise are shown in Figure 5. Except for FP10, all floodplains show an average annual water quality improvement downstream of the corresponding floodplain. It is also noticeable that the extreme cases for improvement and worsening are the FP8 and FP10, respectively.

4.4. Water Quality and Correlation with River Discharge

Complete Pearson’s correlation plots between average yearly nutrient retention and river discharge, as well as correlation plots between water quality improvement and river discharge value are provided in Figures S11–S13. These plots determine the relationship between the discharge values and the water quality. They can also explain the different behaviors of floodplains towards improving the water quality.

4.5. Remote Sensing-Based Machine Learning Models

4.5.1. C2RCC Water Products’ Validation

Correlation between C2RCC and in situ measurements is displayed in Figure 6. Poor results for both Chl-a and TSM products are retrieved, particularly for Chl-a, for which an overestimation occurs in the range of 0–10 mg/L. TSM shows underestimation for almost all the range of the concentration but a slightly better correlation R2 = 0.19. These results justify further modeling using RRS and locally-tuned machine learning approaches in an effort to estimate accurately Chl-a and TSM.

4.5.2. Machine Learning Modeling

After the tuning of hyperparameters, the feature engineering process and the LOOCV, average error metrics were calculated and the three models were compared against each other. Results for Chl-a and TSM are displayed in Table 2 and Table 3. Chl-a ML models perform better with better results for Random Forest R2 = 0.60 and RMSE = 5.90 against SVM (R2 = 0.57 and RMSE = 6.10). TSM ML models perform very poorly, and only LR reach an R2 > 0.10. We chose, therefore, RFR for further estimation of Chl-a and LR for TSM. We assumed, however, that for TSM, we would retrieve highly uncertain results due to the very weak performance of TSM models.

4.5.3. Water Quality Maps

The results of water quality from modeling over the surface of Danube River confirm the previous results from Figure 5. Chl-a spatial variations are shown in Figure 7 for FP2 (Figure 7a), FP6 and FP7 (Figure 7b), and FP8 (Figure 7c). The selected dates of the image acquisition to display spatial variations were based on the time series analysis and WQI analysis. Similarly, TSM spatial variations are shown in Figure 8. From Figure 7, it is visible that upstream regions of FP 2 show a higher concentration of Chl-a (up to 23–27 mg/L), and downstream region reduces its concentration (<=3 mg/L). Similar scenarios are visible in Figure 7b for FP6 and FP7, except for the region at the extreme East, where a plume with high Chl-a concentrations is visible (Figure 7b, downstream). In Figure 7c, a clear difference is visible between upstream and downstream concentrations as well.
Despite the low performance of TSM models, the estimations are in agreement with the average water quality improvement from Figure 5 for FP2 (Figure 8a), FP 6 and FP7 (Figure 8b), and FP 8 (Figure 8c) where upstream higher concentrations are reduced after the floodplain regions.

5. Discussion

5.1. Water Quality and Nutrient Retention

Not all floodplains could be analyzed in our study since there was a lack of field measurements for important nutrients in some stations or an absence of discharge data in other stations.
Floodplains showing a positive behavior in improving the water quality downstream of the floodplain were described to have a low to medium restoration demand, showing that these floodplains’ functionality of filtering contaminants and improving water quality is active, and also, it can be improved further for FP6, FP7, FP8, and FP9, having a medium restoration demand. On the other hand, one floodplain (FP10) did not show a water quality improvement at any year, despite having a medium restoration demand. Still, it is possible that other functionalities are active in this floodplain, such as providing groundwater recharge or supporting habitats, but the improvement of water quality function is not active and needs to be restored.
Moreover, among the floodplains showing a pattern of retaining nutrients, we can notice that 83% of the years in which a flood occurred, the yearly average improvement of water quality was positive. This explains that during flooding years, the water quality improvement function of floodplains is more active.
Regarding the nutrient retention, only five floodplains had enough data to conduct the analysis. Some of the floodplains that showed a retention behavior in the general water quality analysis did not retain nutrients, and also acted quite poor in terms of nutrient retention and vice versa. This is due to other valuable parameters that are taken into consideration when computing water quality, such as Chl-a, TSM, and the Dissolved Oxygen concentrations. Therefore, sometimes, a floodplain may not serve for nutrient retention but it will improve other water quality parameters, leading to a better quality of water downstream.
The poor nutrient retention in floodplains can be caused by a release of nutrients greater than retention capacity. Sometimes, nutrient storages are not permanent due to the dynamic nature of floodplains. Some studies showed floodplains releasing nutrients or sometimes re-suspending them due to scouring currents occurring in the river. Other studies showed a net release of phosphorus or even an increase in both nitrogen and phosphorus amounts in the river channel next to a floodplain [73,74]. Additionally, in some cases, it is important to consider the presence of soluble reactive phosphorus (SRP), which can act disproportionally to downstream eutrophication [21]. Moreover, it is important to consider the nutrients that can be returned to the river via lateral stream migration and erosions from stream banks over long time periods, which can shrink the size of the floodplain each year as well [22,75].
Finally, it is very important to consider river discharge in floodplains because it is the river discharge values that determine the hydraulically connected area of an active floodplain [40]. The correlation between the water quality improvement or the nutrient retention and the river discharge values was not strong, except for some floodplains. In these floodplains, it is important to consider the hydraulic load and the water depth while designing flow rate recommendations for effective treatment, because they play critical roles in the effectiveness of nutrient removal [76]. The poor correlation between discharge rate and retention could be explained by a limited range on the available data and a small difference among inflow concentrations [77]. Finally, some floodplains showed a negative correlation, i.e., showing higher retentions during small river discharges. This can be explained by the fact that during low discharge periods, longer water residence times are expected, promoting nutrient retentions such as denitrification and other types of soil accumulation [78]. Additionally, we have to mention that some floodplains did not have enough sample points in order to do a significant correlation analysis. For example, FP3 and FP9 for both nitrates and phosphorus had only 5 sample points each, which is a small amount of data to make an accurate analysis.

5.2. Machine Learning Models Based on Remote Sensing

Modeling water quality parameters over inland waters, and specifically over large fluvial systems, has been demonstrated to be possible, even when there are challenges and uncertainties associated with the process [79,80]. In this work, the poor correlation with available water products from C2RCC justified further modeling and provide continuous spatial coverage of both Chl-a and TSM. From the error metrics evaluation, Chl-a displayed good performance (R2 = 0.61) and therefore, modeling spatial variation along the river is more certain.
However, TSM performance is very weak (R2 = 0.12), although the spatial patterns are in line with the WQI improvements seen in Figure 5. Still, a complete agreement between these two results is not possible to be demonstrated based on this exercise, since the quality maps represent only one snapshot in a specific moment of interest for the floodplain of interest. Feature engineering was also a useful process that helped to develop better ML models and could be extended in the future.
Although modeling water quality parameters using satellite images and remote sensing has been demonstrated to be possible, we still face many associated challenges and limitations [79,80]. These include the narrow stream channels of a river, requiring a higher spatial resolution of satellite image data [81]. Another challenge is the high variation of sediment concentrations in time and space [81]. Moreover, our modeling was based on remote sensing data, which adds further limitations because of the need to match satellite acquisitions and field measurements. This adds up as a significant limitation in the temporal resolution [79].
Given that Sentinel-2 imagery during the time of interest had a frequency of 1 image every 10 days (low frequency compared to 1 image every 5 days nowadays), a high number of images were eliminated during the filtering process because they did not match the date of field measurements. Other images were eliminated due to cloud cover. This problem can be solved by using multiple satellites. Even so, we believe that the potential of remote sensing is high to evaluate changes in water quality, as done in several studies [34,79], allowing to develop predictive models that can be extrapolated in time (multitemporal analysis) or over space scales (water surface distribution of water parameters).

5.3. Human Intervention and Floodplain Reconnections

Anthropogenic interventions had a direct and major impact on floodplain ecosystems causing them to degrade [76], especially in urban areas. There, the floodplain areas are artificially constructed and therefore show reduced ecosystem functions, due to a loss of connectivity between the river and the historically natural floodplain [82]. In our study, half of the floodplains in the Danube River (especially the upper part) are not fully reconnected [83] and need to be restored. Maximizing the function of a floodplain can be done by fully reconnecting the floodplains and designing them with the optimum river discharge value [77], so that they can retain a higher amount of nutrients from rivers and streams [77].

6. Conclusions and Outlook

Anthropogenic influence has led to disconnected Danube floodplains, which lost 80% of their original size [41], although they are a source of multiple ES. The restoration of lost floodplains is a well-known NbS, used to deal with river water quality issues. We looked for approaches in alternatives to water quality modeling and field measurements, and combined multiple methods to understand the potential of floodplain restoration to improve water quality along the Danube River. The main conclusions on the effect of floodplains on Chl-a, TSM, nitrate nitrogen, total phosphorus, and water quality can be summarized as follows:
  • At the annual scale, most areas downstream of active floodplains have better WQI than the corresponding upstream section, while nitrate and total phosphorus retention do not show a relevant trend (the effect is rather dependent on the single floodplain);
  • There is the need for more sophisticated analyses of remote sensing data, as shown by poor results for in situ validation of Sentinel-2 C2RCC water products; on the other hand, remote sensing-based ML modeling shows more certain results for Chl-a, but is still lacking certainty in the modeling of TSM;
  • The comparison of remote sensing ML approaches (water quality maps) and in situ data analysis (WQI variation shown by the time series) shows an agreement of two independent methodologies.
Based on these observations, we conclude that no homogeneous improvement of water quality downstream of floodplains can be demonstrated with the applied methodologies (data series analysis and remote sensing-based ML), due to missing statistical relevance of the data. Therefore, we can only partially determine the benefits of floodplains along the Danube River.
More effort should be put into predicting the potential of floodplains for water quality improvement. One way to do so is the study of active floodplains and their effects on water quality, as done in this work at the full river-length scale. Other ways to predict the potential of nutrient retention are to work at the floodplain scale by implementing in situ measurements [84], or to conduct water quality modeling, as done in multiple ways in the Danube River Basin [85,86,87,88]. Instead of focusing on only one of these approaches, we recommend researchers to combine their skills and efforts to conduct interdisciplinary work, so that methodologies based on different backgrounds can be compared, and results can be double-checked. For example, spatially highly dense sub-daily field measurements implemented on one floodplain could be combined with physically-based or statistical models for upscaling calibrated parameters on a whole river basin.
Water quality estimations on rivers based on remote sensing still presents some limitations [79], such as the low performance of the models for TSM, or the dependence on the temporal resolution of the chosen satellites. Nevertheless, this publication is, to the authors’ knowledge, the first attempt to analyze floodplain benefits in terms of water quality through a holistic set of approaches, which also includes satellite remote sensing. We call for other researchers, as done by Zhang et al. [80] or Peterson et al. [79], to explore the potential of remote sensing to evaluate floodplains’ ecosystem services, not only limiting to nutrient retention, but also analyzing carbon sequestration, flood mitigation, or nature-based recreation.
Additionally, future research should focus on developing other ML techniques with hydrological and remote sensing applications, such as the extreme learning machine (ELM), or hybrid methods such as the hybrid back propagation neural network (BPNN). ELM has demonstrated to produce high accurate models that can provide stakeholders with important and precise sediments’ information with a continuous and finer spatial resolution [79]. In addition, ELM outperformed traditional monitoring methods, leading to better results [79]. Moreover, ELM can be further refined with Sentinel-2 sensors, resulting in finer and more accurate estimates of concentrations [79]. On the other hand, hybrid methods such as the hybrid BPNN can be trained with a little amount of data and still outperform other models [80]. In conclusion, ML still has a lot of room for improvement, especially in hydrological applications, and further studies should be made to improve ML models in remote sensing.
For future analyses on floodplain restoration NbS, special attention should be put into further estimating the effect of hydrological connectivity, as this has been shown to be a main driver determining the amounts of nutrients retained by floodplains [88]. In fact, frequent inundations and complete reconnection of side arms would lead to higher nutrient retention [88], and simultaneously increase typical floodplain habitat provisioning, whose degree of biodiversity and primary productivity is higher than purely terrestrial or aquatic ecosystems [89]. In fact, even with less than 2% of Earth’s land surface, floodplains furnish nearly 25% of all ES, excluding marine ecosystems [90].
Finally, more investments should be put into the restoration of floodplains and other ecosystems, such as peatlands and forests, as, for example, announced for Germany with the Action Program “Natural Climate Protection” by the Federal Government, which plans to invest 4 billion Euros for NbS for climate protection between 2022 and 2026 [91].

Supplementary Materials

The following supporting information can be downloaded at https://www.mdpi.com/article/10.3390/hydrobiology1020016/s1, Figure S1: Time series plots for floodplain 1 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S2. Time series plots for floodplain 2 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S3. Time series plots for floodplain 3 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S4. Time series plots for floodplain 4 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S5. Time series plots for floodplain 5 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S5. Time series plots for floodplain 5 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S6. Time series plots for floodplain 6 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S7. Time series plots for floodplain 7 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S8. Time series plots for floodplain 8 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S9. Time series plots for floodplain 9 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S10. Time series plots for floodplain 10 showing the concentration of: (a) Nitrates, (b) Total Phosphorus, (c) Chlorophyll-a and (d) TSM, Figure S11. Correlation between the Nitrogen Retention and the water discharge values for: (a) FP1, (b) FP2, (c) FP3, (d) FP9 and (e) FP10, Figure S12. Correlation between the Phosphorus Retention and the water discharge values for: (a) FP1, (b) FP2, (c) FP3, (d) FP9 and (e) FP10, Figure S13. Correlation between the water quality improvement and the water discharge values for: (a) FP2, (b) FP6 and (c) FP10.

Author Contributions

Conceptualization, F.P. and L.F.A.-R.; methodology, F.P. and L.F.A.-R.; software, validation, formal analysis, investigation, resources, data curation, writing—original draft preparation A.H., writing—review and editing, visualization, supervision, project administration, F.P. and L.F.A.-R. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Data Availability Statement

The data derived from the Danube River Basin Water Quality Database are not available to the public.

Acknowledgments

We would like to thank all Danube Floodplain project’s partners for providing necessary input data and useful insights regarding the study areas, especially the International Commission for the Protection of the Danube River (ICPDR), the University of Szeged (USZ), and the University of Natural Resources and Life Sciences (BOKU). Additionally, we would like to thank the Chair of Hydrology and River Basin Management (Disse) of the Technical University of Munich for providing administrative and technical support. We thank the peer reviewers for providing constructive comments, which extensively improved this manuscript. Finally, we would like to thank the Mexican National Council for Science and Technology (CONACYT).

Conflicts of Interest

The authors declare no conflict of interest.

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Figure 1. The active floodplains (FP) of the Danube River used in this study.
Figure 1. The active floodplains (FP) of the Danube River used in this study.
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Figure 2. Flowchart describing the methodology applied in this work.
Figure 2. Flowchart describing the methodology applied in this work.
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Figure 3. WQI percentual improvement and river discharge time series in: (a) FP2; (b) FP3; (c) FP6; (d) FP7; (e) FP8; (f) FP9; (g) FP10.
Figure 3. WQI percentual improvement and river discharge time series in: (a) FP2; (b) FP3; (c) FP6; (d) FP7; (e) FP8; (f) FP9; (g) FP10.
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Figure 4. Average yearly retention values of the analyzed floodplains (FP) for: (a) Nitrogen; (b) Phosphorus.
Figure 4. Average yearly retention values of the analyzed floodplains (FP) for: (a) Nitrogen; (b) Phosphorus.
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Figure 5. Average yearly water quality improvement of the analyzed floodplains (FP).
Figure 5. Average yearly water quality improvement of the analyzed floodplains (FP).
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Figure 6. In situ validation for Case 2 Regional Coast Color (C2RCC) algorithm results with in situ measurements: (a) Chlorophyll-a (Chl-a); (b) Total Suspended Matter (TSM).
Figure 6. In situ validation for Case 2 Regional Coast Color (C2RCC) algorithm results with in situ measurements: (a) Chlorophyll-a (Chl-a); (b) Total Suspended Matter (TSM).
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Figure 7. Water quality maps for Chlorophyll-a expressed in mg/L for the three areas that correspond to (a) floodplain 2 (S2 image acquired on: 13 April 2016); (b) floodplains 6 and 7 (S2 image acquired on: 28 February 2017); (c) floodplain 8 (S2 image acquired on: upstream on 26 May 2017 and downstream on 15 May 2017). Basemap: ESRI Gray. EPSG: 3857.
Figure 7. Water quality maps for Chlorophyll-a expressed in mg/L for the three areas that correspond to (a) floodplain 2 (S2 image acquired on: 13 April 2016); (b) floodplains 6 and 7 (S2 image acquired on: 28 February 2017); (c) floodplain 8 (S2 image acquired on: upstream on 26 May 2017 and downstream on 15 May 2017). Basemap: ESRI Gray. EPSG: 3857.
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Figure 8. Water quality maps for total suspended matter (TSM) expressed in mg/L for the three areas that correspond to (a) floodplain 2 (S2 image acquired on: 13 April 2016); (b) floodplains 6 and 7 (S2 image acquired on: 28 February 2017); (c) floodplain 8 (S2 image acquired on: upstream on 26 April 2017 and downstream on 15 May 2017). Basemap: ESRI Gray. EPSG: 3857.
Figure 8. Water quality maps for total suspended matter (TSM) expressed in mg/L for the three areas that correspond to (a) floodplain 2 (S2 image acquired on: 13 April 2016); (b) floodplains 6 and 7 (S2 image acquired on: 28 February 2017); (c) floodplain 8 (S2 image acquired on: upstream on 26 April 2017 and downstream on 15 May 2017). Basemap: ESRI Gray. EPSG: 3857.
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Table 1. Floodplain keywords, locations, upstream and downstream gauging stations, morphometric data, and their restoration demand, as assessed according to the Danube Floodplain Project [40].
Table 1. Floodplain keywords, locations, upstream and downstream gauging stations, morphometric data, and their restoration demand, as assessed according to the Danube Floodplain Project [40].
Floodplain KeywordRestoration DemandLocationArea Size (km2)Floodplain Length (km)River Kilometer (km)CountriesUpstream Stations CodeDownstream Stations Code
FP1High48.144° N 17.025° E19.89.81880–1871.5Austria
Slovakia
AT6AT4
SK1
FP2Low47.889° N 17.476° E140.251.41851.8–1797Hungary
Slovakia
AT4
SK1
HU1
SK2
FP3Low45.614° N 18.905° E279.970.11425–1354.2Serbia
Croatia
HU5
HR1
HR2
RS2
FP4 *High
Medium
45.323° N 19.084° E
45.268° N 19.226° E
24.6
30
16.8
9.3
1334–1318
1318–1308.4
Serbia
Croatia
HR2
RS2
RS9
HR11
FP5High
High
45.235° N 19.485° E49.227.21304–1276Serbia
Croatia
RS9
HR11
RS3
45.224° N 19.729° E34.816.81276–1258
FP6 *Medium
Medium
43.779° N 23.811° E
43.716° N 24.069° E
60.1
32.3
25.2
15.6
703–677
677–661
Bulgaria
Romania
RO18
RS8
RO2
BG1
BG2
FP7 *Medium
Medium
43.736° N 24.433° E29.315.4646–630Bulgaria
Romania
BG2BG11
BG3
43.725° N 24.697° E81.630.9630–600
FP8Medium43.911° N 26.033° E25.310.3490–479.5Bulgaria
Romania
BG4RO3
BG8
BG15
FP9Medium44.136° N 26.93° E33.614.9412–395.5Bulgaria
Romania
RO3RO4
BG5
FP10 *Medium
Medium
Low
Low
44.125° N 27.37° E
44.226° N 27.714° E
44.475° N 28.031° E
44.901° N 27.903° E
50.3
79.4
93.6
298.8
17.7
31.2
58.6
77.9
375–356
345–313.5
313.5–252.5
252.5–172
RomaniaRO4
BG5
RO11
RO5
UA1
* Some of the floodplains consist of multiple floodplains combined and analyzed together.
Table 2. Machine learning models’ results for best runs of each algorithm for Chl-a estimation.
Table 2. Machine learning models’ results for best runs of each algorithm for Chl-a estimation.
R2RMSENumber of Features
MLR0.317.761
RF0.605.902
SVR0.576.105
Table 3. Machine learning models’ results for best runs of each algorithm for TSM estimation.
Table 3. Machine learning models’ results for best runs of each algorithm for TSM estimation.
R2RMSENumber of Features
MLR0.1215.621
RF0.0815.992
SVR0.0821.071
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Hoyek, A.; Arias-Rodriguez, L.F.; Perosa, F. Holistic Approach for Estimating Water Quality Ecosystem Services of Danube Floodplains: Field Measures, Remote Sensing, and Machine Learning. Hydrobiology 2022, 1, 211-231. https://doi.org/10.3390/hydrobiology1020016

AMA Style

Hoyek A, Arias-Rodriguez LF, Perosa F. Holistic Approach for Estimating Water Quality Ecosystem Services of Danube Floodplains: Field Measures, Remote Sensing, and Machine Learning. Hydrobiology. 2022; 1(2):211-231. https://doi.org/10.3390/hydrobiology1020016

Chicago/Turabian Style

Hoyek, Alain, Leonardo F. Arias-Rodriguez, and Francesca Perosa. 2022. "Holistic Approach for Estimating Water Quality Ecosystem Services of Danube Floodplains: Field Measures, Remote Sensing, and Machine Learning" Hydrobiology 1, no. 2: 211-231. https://doi.org/10.3390/hydrobiology1020016

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