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Comment on “Soil salinity assessment by using near-infrared channel and Vegetation Soil Salinity Index derived from Landsat 8 OLI data: a case study in the Tra Vinh Province, Mekong Delta, Vietnam” by Kim-Anh Nguyen, Yuei-An Liou, Ha-Phuong Tran, Phi-Phung Hoang and Thanh-Hung Nguyen
Progress in Earth and Planetary Science volume 9, Article number: 45 (2022)
Nguyen et al. (Prog Earth Planet Sci 7:1, 2020. https://doi.org/10.1186/s40645-019-0311-0) suggest that Landsat 8 OLI can be used to map and monitor soil salinity in the coastal zone of the Mekong River Delta. The authors use empirical correlations between the near-infrared (NIR) band, or vegetation indexes containing the NIR band, and soil salinity. We show that within the coastal portion of the Mekong Delta, extensively ponded due to widespread shrimp farming, about 90% of Landsat 8 pixels are fully or partially covered by water. We then find that, due to strong NIR radiation absorption, NIR reflectance from ponded pixels decreases linearly with increasing water percentage cover, while no significant correlation is found between reflectance and soil salinity. Through detailed new analyses, we conclude that NIR reflectance attenuation cannot be ascribed to vegetation stress caused by soil salinity, but rather to the presence of water ponds. We also show that a similar behavior exists in ponded freshwater inland areas, confirming that the NIR absorption exerted by water is independent of salinity.
Nguyen et al. (2020) suggest that soil salinity can be monitored using Landsat 8 OLI (L8 hereafter) in the coastal zone of the Mekong River Delta. The study suggests an inverse exponential correlation between the near-infrared (NIR) band (i.e., L8 band-5) and the electrical conductivity (EC1:5) (i.e., determined using a conductivity probe on a mix of 1 part soil with 5 parts deionized water) determined at several points within their study site (Tra Vinh Province, Fig. 6 plot d of Nguyen et al. 2020). Significant correlations between vegetation indexes that include the NIR band and soil EC1:5 are also highlighted in the study (see Fig. 8 plots SI4, NDSI, NDVI, SAVI and VSSI of Nguyen et al. 2020). The authors underline the good performance of the Vegetation Soil Salinity Index (proposed by Dehni and Lounis (2012) as VSSI = 2 × green − 5 × (red + NIR), where “green” and “red” are the L8 band-3 and the L8 band-4, respectively).
The Tra Vinh Province covers a large territory that includes inner agricultural lands as well as a coastal wetland zone, characterized by an extensive presence of ponds for shrimp farming (Wassmann et al. 2019). Focusing exclusively on the latter, we will show in this comment article that (1) L8 spatial resolution is not suitable to distinguish between ponded and non-ponded areas; therefore, (2) the decreased NIR reflectance ascribed to increased soil salinity is instead due to the presence of water in L8 mixed pixels. Finally, (3) we show that NIR reflectance is equally reduced independently of whether the water ponding area is saltwater or freshwater.
Salinity affects vegetation development and its health status. Some vegetation species, as halophytes, can grow on salt marsh salted soil because they developed specific adaptation measures (Silvestri and Marani 2004). Mangroves are also highly tolerant to salinity, thanks to a range of adaptations (Parida and Jha 2010). However, in areas other than coastal saline wetlands, salt is toxic to vegetation and affects the development of natural vegetation as well as crop production (Montanarella et al. 2015; Vargas et al. 2018). Hence, in these cases, remote sensing can be used to detect the stress that salt produces on plants, causing lower photosynthetic activity (Tilley et al. 2007; Zhang et al. 2015; Scudiero et al. 2015). Specifically, decreased near-infrared (NIR) reflectance is observed when vegetation is subjected to salinity stress (Wang et al. 2002; Tilley et al. 2007; Zhang et al. 2011). L8 has been used for this purpose in other studies (Scudiero et al. 2015; Gorji et al. 2020). However, factors other than salinity stress may be responsible for a reduction in NIR reflectance, as the presence of water around or underneath the vegetation, a well-known effect in wetlands (Silva et al. 2008; Hestir et al. 2008; Adam et al. 2010). Therefore, the conclusion that a reduction in the NIR reflectance is due to vegetation stress caused by increased salinity must be carefully tested in coastal wetlands, and the influence of water absorption must be accounted for (Dekker et al. 2002).
Here, we focus on the same L8 OLI image analyzed by Nguyen et al. (2020), acquired on February 14, 2017, and available in USGS EarthExplorer. We selected the Collection-2 Level-2 product (see detailed characteristics in Additional file 1: Table S1), which is geometrically, radiometrically and atmospherically corrected to surface reflectance by USGS (2022). We masked the areas covered by clouds.
Landsat 8 OLI spatial resolution is not adequate to study soil salinity in the ponded coastal zone of the Mekong River Delta
Wetlands are characterized by partly emerged and submerged areas. The coastal portion of the Mekong River Delta is characterized by an almost continuous presence of artificial ponds, mainly used for shrimp farming (Fig. 1). Ponds are surrounded by embankments with little streets, small villages, bare soil as well as vegetated areas. In order to identify emerged vegetation and study its health status, the spatial resolution allowing pixels to be mostly “pure” (i.e., either exclusively composed of fully emerged or fully submerged areas) should first be determined. Too coarse resolution, in fact, gives a large percentage of mixed pixels, i.e., pixels comprising both emerged and flooded areas, with a reflectance that is intermediate between those from both categories. To understand if Landsat data can be used to discriminate ponded vs non-ponded surfaces, we must determine the probability that pixels contain portions of standing waters. We can perform such analysis by generating a grid with cells of 30 m × 30 m, overlaying on L8 pixels, and by counting the number of cells that fully fall on water ponds, land and mixed water/land areas. Since the coastal ponded area within the Tra Vinh Province is very large (more than 275 km2, see Fig. 1), we performed these analyses by generating 20 grids of 10 × 10 cells (of 30 m × 30 m each) distributed across the ponded area. Twelve grids were created around the sampling points described in Nguyen et al. (2020; points with IDs 30–41 listed in Table 4), while other eight grids were randomly generated in QGIS across the remaining ponded area (Fig. 1). The detection of the grid cells falling on water ponds or on emerged land was determined with a visual inspection method in QGIS using Google Earth satellite as base image. Google Earth is the most accurate high-resolution virtual globe currently available and covers almost the entire land surface of the Earth (Yu and Gong 2012; Guo et al. 2020). It integrates aerial photographs with medium to high spatial resolution satellite images mainly collected by WorldView-1/2/3, GeoEye-1, Airbus' Pleiades, QuickBird, Landsat and SPOT5. Such integration allows the operator to zoom to around 0.3–0.5 m resolution (see Additional file 1: Table S2 for details) depending on the availability of satellite images in different locations of the world. Therefore, the advantage of using Google Earth is that it provides a recent cloud-free base image with an extremely high spatial resolution that allows the operator to clearly detect water ponds and land. The horizontal accuracy of Google Earth varies for different locations of the world and is strongly affected by topography, being lower on mountainous terrain and higher on plains. Several studies have shown that on plains and lowlands the absolute positioning accuracy generally varies between 0.1 and 5.0 m (Benker et al. 2011; Paredes-Hernandez et al. 2013; Goudarzi and Landry Jr 2017; Guo et al. 2020). The disadvantage is that Google Earth is a collage of images collected very recently but in different periods, and some land-use changes may have occurred since 2017, when the L8 image used in this study was acquired. Some differences may also be due to seasonal variations or differences in water levels. Moreover, given the typically high humidity of the Mekong delta, some areas are still covered by clouds. Therefore, to further verify the method, we also used Google Earth Pro to explore the database of available images, including those collected before February 2017, by overlaying the same 20 grids generated in QGIS. Figure 1 shows an example of two generated grids, while Table 1 shows the number of cells that, within each grid of 10 × 10 cells, fully fall within water ponds, land or on mixed surfaces using the recent Google Earth image as well as cloud-free images collected before February 2017. The table includes the dates of the analyzed images. We notice that, on average, more than 86% of the cells contain both water and emerged areas, and almost 4% fall on water ponds, confirming that the large majority of L8 pixels are affected by the presence of water.
Pixels that fully or partially fall on water bodies are affected by the water ability to absorb incident energy in the infrared portion of the electromagnetic spectrum, attenuating the reflected NIR signal (see Dekker et al. 2002) and therefore interfering with any possible signal attenuation linked to vegetation stress. Our results indicate that in the ponded coastal area of the Tra Vinh Province, about 90% of the Landsat pixels are affected by the presence of water and should be masked to avoid the NIR reflectance attenuation exerted by water. Only the remaining 10% can be used to study a possible correlation between soil salinity and NIR reflectance, using salinity field measurements performed exclusively within pixels that fully fall on emerged land. This method would provide a map with more than 90% of masked pixels. Therefore, we conclude that L8 spatial resolution is not suitable for this purpose in the ponded coastal area of the Tra Vinh Province. High spatial resolution satellites, such as WorldView-3 or Planet, would provide a much larger number of pixels falling on emerged land, allowing a more effective analysis.
The presence of ponds influences the NIR signal (and the vegetation indexes containing NIR), masking possible relations with soil EC1:5 in the coastal area of the Tra Vinh Province
We selected twelve L8 pixels corresponding to the field measurement points described in Nguyen et al. (2020) across the coastal area (points with IDs 30–41 listed in Table 4). The location of the twelve points can be seen in Additional file 1: Fig. S1. We notice that the points fall on embankments surrounded by ponds and channels and that eleven out of the twelve L8 OLI pixels corresponding to the sampling points fall on mixed water/land surfaces (Additional file 1: Fig. S1). We notice that two points (point G30 and point G41) fall at the edge between land and water, and point G40 falls on water, even though very close to the embankment. This may be due to a low precision of the Global Navigation Satellite System (GNSS) receiver used by the authors or to a low absolute positioning accuracy of the Google Earth images as discussed in the previous chapter. Nevertheless, we underline that an error of a few meters in the relative positioning of GNSS points is small with respect to the size of the L8 pixels themselves. We notice that in all cases, pixels and their nearest neighbors contain a very high proportion of water. In order to quantify the water percentage cover within each selected pixel, we generated 100 regularly spaced points (see Additional file 1: Fig. S2). As we did for the analysis described at paragraph 2.1, we used recent and historical Google Earth satellite images (see Table 1 for image dates) to visually determine the number of points falling on water ponds (Additional file 1: Fig. S2). This number is the best available proxy of actual water percentage cover. Figure 2a shows that there is a significant linear correlation (P value < 0.01) between the water percentage cover and the L8 NIR band reflectance: Reflectance decreases with increasing water percentage cover, confirming that shrimp farming ponds interfere with the reflectance signal, by absorbing near-infrared electromagnetic energy. This correlation is slightly stronger if we consider the values of water percentage cover determined using historical images in Google Earth. No significant correlation could be found between EC1:5 and the L8 NIR reflectance (Fig. 2). We also performed a multiple regression of L8 NIR reflectance on EC1:5 and water percentage cover as independent variables. We find that L8 NIR reflectance variability is almost totally explained by water percentage cover, while the correlation with EC1:5 is not significant (P value > 0.05). A similar behavior is observed when considering the VSSI as a dependent variable instead of the NIR reflectance.
The presence of ponds reduces NIR reflectance whether they contain saltwater or freshwater
In order to explore the possible influence of salt on the previous analysis, we compared the effect of the water presence on the NIR reflectance in freshwater and saline ponded environments. Therefore, we randomly selected 20 pixels falling on freshwater ponds in the inner Mekong River Delta, at a distance higher than 60 km from the mouth (Fig. 1), so that the ponds are not affected by salinity (Eslami et al. 2019; Wassmann et al. 2019). As for the coastal saline area, in order to match the 20 observations selected in the freshwater area, to the original 12 pixels corresponding to the field observations performed by Nguyen et al. (2020), we added 8 pixels randomly selected within the grids used to determine if the L8 spatial resolution were adequate (Fig. 1). We generated 100 points regularly spaced within all the created pixels. Figure 3 shows that in (a) saltwater ponded areas as well as in (b) freshwater ponded areas, there is a significant linear correlation (P value < 0.01) between water percentage cover and reflectance of the L8 NIR band. Similarly, Fig. 3 shows that there is a significant linear correlation (P value < 0.01) also between water percentage cover and the VSSI for (c) saltwater and (d) freshwater ponded areas. Our results confirm that NIR reflectance is gradually reduced by an increasing water surface, in both salted and freshwater environments. This result confirms that salinity does not influence the absorption of the incident energy exerted by water.
Nguyen et al. (2020) has the merit of exploring the use of L8 OLI to study the influence of salinity on vegetation in the Mekong River Delta. Even though the L8 spatial resolution is suitable to perform the analysis on the inner agriculture land of the Tra Vinh Province considered by the authors, we show that the method cannot be applied to the coastal area where shrimp farming ponds are widely present. We have shown that L8 spatial resolution is not suitable to distinguish between ponded and non-ponded areas in the coastal portion of the Tra Vinh Province, because about 90% of the L8 pixels fully or partially fall on ponds and canals. We have also shown that the attenuation of the NIR reflectance is primarily due to the water presence and decreases linearly with increasing water percentage cover, while no significant correlation between soil salinity and NIR reflectance could be found. The attenuation of the NIR reflectance due to the presence of water ponds is similar in the coastal saline area and in the inner freshwater area.
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Diep Nguyen Ngoc and the collaboration among the authors were supported by the European Commission under the Erasmus Mundus Joint Master Degree Programme in Water and Coastal Management [Grant Number 586596-EPP-1-2017-1-IT-EPPKA1-JMDMOB]. The authors would like to acknowledge the anonymous reviewers of this article who gave an important contribution to improve it.
European Commission under the Erasmus Mundus Joint Master Degree Programme in Water and Coastal Management [Grant Number 586596-EPP-1-2017-1-IT-EPPKA1-JMDMOB].
This article does not contain any studies with human participant or animals performed by any of the authors.
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Silvestri, S., Nguyen, D.N. & Chiapponi, E. Comment on “Soil salinity assessment by using near-infrared channel and Vegetation Soil Salinity Index derived from Landsat 8 OLI data: a case study in the Tra Vinh Province, Mekong Delta, Vietnam” by Kim-Anh Nguyen, Yuei-An Liou, Ha-Phuong Tran, Phi-Phung Hoang and Thanh-Hung Nguyen. Prog Earth Planet Sci 9, 45 (2022). https://doi.org/10.1186/s40645-022-00490-7
- Soil salinity
- Mekong River Delta
- Coastal areas
- Landsat 8 OLI
- Google Satellite
- Near-infrared reflectance reduction
- Water absorption
- Mixed pixels