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Soil Moisture Mapping of Solano Nueva Vizcaya: A Comparison and
Review
Sarilyn R. Lopez, Eirene Allaizza C. Reyes
Department of Geodetic Engineering, Nueva Vizcaya State University, Bayombong, Philippines
DOI:
https://doi.org/10.51583/IJLTEMAS.2026.150400004
Received: 26 March 2026; 01 April 2026; Published: 27 April 2026
ABSTRACT
Soil moisture, defined as the presence or amount of water in the soil, is a critical element in hydrology,
agriculture, and climate science, vital for understanding soil health, water cycle, and plant growth. Remote
sensing, particularly using satellites like Sentinel-2 which is equipped with Multispectral instruments, offers a
powerful tool for monitoring soil moisture across large areas. Therefore, this study was conducted to generate
soil moisture maps of Solano Nueva Vizcaya through Geographic Information System by using Sentinel-2 Near
InfraRed and Short Wavelength InfraRed bands for the years 2020 and 2025. It further aimed to determine the
soil moisture level of the study area and compare soil moisture level differences between the years 2020 and
2025, and at the same time identify the minimum, maximum, and the mean soil moisture per barangay. The
results revealed that the municipality of Solano has a minimum soil moisture level increased by 0.304678159,
while the maximum decreased by 0.062563121. It was also revealed that most of the dry soil are located within
the lowland areas and generally the results indicate a general increasing trend in soil moisture in Solano for the
years 2020 and 2025.
Keywords: Near InfraRed, Sentinel-2, Short Wavelength InfraRed, Soil Moisture
INTRODUCTION
One important element in the scientific and engineering field including hydrology, agriculture, and climate
science, is soil moisture. It is referred as the presence or amount of water in the soil, which is very important for
understanding soil health, water cycle, and plant growth (Jackson & Hsu, 2004). The great needs for measuring
soil moisture content also extends for the purpose of water management, prediction of crop yield, and climate
modelling. Traditionally, ground-based methods are mainly used to measure soil moisture, but because of the
use of modern technology such as remote sensing instruments, the ability to monitor soil moisture in larger scales
have improved (Entekhabi et al., 2010).
Evidences of the importance of soil moisture can be seen across different fields. In agriculture, influencing crop
growth and yield, hence considered important for the optimization of irrigation practices and ensuring food
security (Jackson & Hsu, 2004). In hydrology, soil moisture is also important as it affects water infiltration,
recharge of groundwater, and runoff. Also, soil moisture is a very important element in energy fluxes and rate of
evaporation, which justifies its benefit in the field of climate science (Entekhabi et al., 2010).
Remote sensing provides a powerful tool for measuring soil moisture content across extensive geographic
regions, overcoming the limitations of ground-based observations (Rizzi, 2022). Satellites equipped with
specialized instruments use electromagnetic waves to infer soil moisture levels from space. Active microwave
sensing, passive microwave sensing, and optical and infrared sensing are the main remote sensing techniques
which are used for soil moisture measurement (NASA MODIS, 2023).
Sentinel-2 satellites can be used for estimating soil moisture given its optical and multispectral sensors. Sentinel-
2 satellites are part of the Copernicus program launched by the European Space Agency. Multispectral
Instruments (MSI) are installed within these satellites enabling them to capture data across 13 spectral bands
which ranges from the visible to the shortwave infrared. The resolution for visible and near-infrared bands is 10
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meters while the shortwave infrared band has a resolution of 20 meters. One spatial index that can be used in
estimating the soil moisture which can be derived from Sentinel- 2 data is the Normalized Difference Moisture
Index (NDMI). For this index, the NIR and SWIR specifically the bands 8a and 11 are used to calculate the soil
moisture level. If the calculated value is high, it generally indicates higher soil moisture levels, on the other hand,
drier conditions can be associated with lower values (ESA, 2022).
By integrating NDMI data derived from the Sentinel-2 satellite and processing it through GIS software, a
relatively accurate soil moisture estimate can be achieved, and the results can be projected through a soil moisture
map. Moreover, the researcher can identify which part of the land cover of Solano has dry to wet soil, which can
be used for various purposes such as flood and drought monitoring with the following objectives: to generate a
comprehensive GIS-based soil moisture map using Sentinel-2 Multispectral Index showing the soil moisture
levels of Solano, Nueva Vizcaya for the years 2020 and 2025; to compare the differences in terms of soil moisture
level between the year 2020 and 2025 for the whole municipality of Solano; and to identify the minimum,
maximum, and mean values of the soil moisture per barangay for the years 2020 and 2025.
METHODOLOGY
Research Design
This study utilized a qualitative research design to generate a soil moisture index map of the study area.
Geospatial data, such as the Near Infrared band and Shortwave Infrared band, was collected as a secondary data
through the Sentinel’s opensource website. Moreover, the detailed explanation of the soil moisture index map is
descriptive and illustrative in nature.
Conceptual Framework
The conceptual framework illustrates the input, process, and output of the study. The figure shows that the inputs
are Sentinel-2 data from Copernicus website specifically the band 8A or the Near Infrared band, and the band 11
or the Shortwave Infrared band. These bands are crucial for calculating the Normalized Difference Moisture
Index (NDMI) which is indicative of soil moisture content. The first process is the data preprocessing which was
executed using the Sentinel- 2 Copernicus Website, where accessing of the Sentinel Level 2A data, clipping of
the imagery to the study area, and cloud masking to enhance the accuracy of the satellite data by removing cloud
interferences was performed. The next process is the creation of thematic map which was conducted in ArcGIS
10.8 to visualize the spatial distribution of soil moisture across the study area. This step involves creating detailed
maps that depict varying levels of soil moisture, thus providing valuable insights into the spatial variability
within Solano, Nueva Vizcaya.
Figure 1. Conceptual Framework of the study
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Research Locale
Solano is a 1st-class municipality in the province of Nueva Vizcaya, situated in the Cagayan Valley region of
Luzon, Philippines, located approximately at coordinates 16°31'N latitude and 121°11'E longitude. The
municipality has an elevation ranging from approximately 240 meters to 573 meters above sea level. Solano
encompasses a total land area of 139.80 square kilometers divided into 22 barangays. The landscape of Solano
is characterized by a mix of rolling hills and agricultural plains, with the Magat River and its tributaries playing
a significant role in the local ecosystem and agricultural practices. Similar to the broader region, Solano
experiences a tropical monsoon climate with pronounced wet and dry seasons. The wet season typically occurs
from June to October, while the dry season runs from November to May. Temperatures generally range from the
low 20s to low 30s degrees Celsius throughout the year, with the warmest months typically being April and May
and the coolest months being December and January.
Figure 2. Location Map of Solano, Nueva Vizcaya
Research Instrument
In this study, the researcher utilized the Sentinel- 2 Copernicus for the preprocessing of data. This involves cloud
masking to identify and exclude cloud-covered areas in the satellite images, as clouds can interfere with the
accuracy of the soil moisture index to detect and mask clouds, ensuring only clear-sky pixels are used in the
analysis. Moreover, the software ArcGIS 10.8 was used as the primary tool for data processing, mapping, and
analysis, which will include the importing of the TIFF file exported from Sentinel- 2 Copernicus, and creation
of the thematic map.
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Data Gathering Procedure
The data gathering procedure involved acquiring geospatial data for spatial analysis. The first step in the data
gathering procedure involved acquiring satellite imagery from the Copernicus Open Access Hub, which provides
free access to Sentinel-2 imagery. The researcher then specified Solano, Nueva Vizcaya, as the Area of Interest
(AOI) by uploading a shapefile of the study area. The temporal filters were then set to select imagery from the
specific time period. Next, the data filters were applied to select Sentinel-2 imagery, focusing on Level-2A
(Bottom-Of-Atmosphere or BOA reflectance) products, which are reflectance values corrected for atmospheric
effects, providing surface reflectance values at the bottom of the atmosphere. Once suitable images were
identified, the data was then gathered by downloading the file. Since this study is delimited only to using
Sentinel-2 satellite data, without incorporating ground-based measurements for validation or comparison,
ground-based measurements are not used.
Statistical Tool
In this study, the researcher used zonal statistics as a suitable statistical tool to facilitate the analysis of the soil
moisture data. Zonal statistics involves dividing the study area into smaller, more homogeneous zones and then
calculating the average soil moisture content within each of these zones. This method was used for the whole
municipality of Solano dividing the zones per barangay. Using zonal statistics, the researcher was able to present
the mean data per barangay level to facilitate a descriptive analysis where the characterization and comparison
of the NDMI values will be done in order to identify the soil moisture conditions across the study area.
For Problem 1, the researcher utilized ArcGIS 10.8 to generate a comprehensive GIS-based soil moisture index
map of Solano using Sentinel-2 spectral bands 8A and 11, and analyze variations in soil moisture across the
study area for the years 2020 and 2025.
For Problem 2, the researcher compared the mean, minimum, and maximum soil moisture levels of the whole
municipality for the years 2020 and 2025, and descriptively drew conclusion based on the compared values.
For Problem 3, the researcher used the in-system tool in Sentinel-2 Copernicus to compute for the mean,
minimum, and maximum soil moisture values per barangay for the years 2020 and 2025.
Statistical Analysis and Procedures
The creation of soil moisture index map involved the application of spatial analysis tools in ArcGIS 10.8. The
following provides a concise description of the procedural steps that will be followed to generate the soil
moisture index map.
After importing the TIFF data from the Sentinel-2 Copernicus consisting of the necessary Sentinel-2 spectral
bands, the Clip tool from the Geoprocessing toolbox was used to focus on the study area. The Project Raster tool
was then utilized to ensure that the data is in the correct coordinate system. Next, the composite band tool was
used to merge the spectral bands and make one layer of data. Since ground-based measurement will not be used,
regression analysis is not required.
The Sentinel-2 Copernicus was again used to calculate for the mean, minimum, and maximum values both for
the whole municipality and barangay level for the years 2020 and 2025. The downloaded data was then imported
in ArcGIS to complete the needed data for the thematic map.
The researcher then applied appropriate symbology and choose a color ramp that effectively represents soil
moisture levels. After all these steps, supplementary steps was done to design the final map layout for this
thematic map, the Kriging Interpolation was applied with a spatial resolution of 10 meters by 10 meters.
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RESULTS
Soil moisture variation across Solano as observed from the Sentinel-2 imagery in the years 2020 and 2025
Table 1. Classification of Soil Moisture Levels
Soil Moisture Value
Soil Moisture Classification
-1 to -0.2
DRY SOIL
-0.2 to 0.4
OPTIMUM MOISTURE
0.4 to 1
WET SOIL
The minimum, maximum, mean values, and classification of the soil moisture per barangay for the years
2020 and 2025
Table 3. Soil moisture values, rank, and classification of each barangay of the municipality of Solano
for the year 2020
Barangay
Minimum
Mean
Rank
Soil Moisture
Classification
Aggub
-0.192015454
0.110687895
19
th
Lowest
Optimum Moisture
Bagahabag
-1
-0.267025207
5
th
Lowest
Dry Soil
Bangaan
-0.144397259
0.10977656
18
th
Lowest
Optimum Moisture
Bangar
-0.681604651
-0.415830947
3
rd
Lowest
Dry Soil
Bascaran
-0.174167067
0.040938806
9
th
Lowest
Optimum Moisture
Communal
-0.166549042
0.136868489
21
st
Lowest
Optimum Moisture
Concepcion
-0.195654988
0.116039713
20
th
Lowest
Optimum Moisture
Curifang
-0.213046491
0.035785189
8
th
Lowest
Optimum Moisture
Dadap
-0.776470637
-0.652269548
1
st
Lowest
Dry Soil
Lactawan
-0.116688304
0.092438991
16
th
Lowest
Optimum Moisture
Osmeña
-0.190005809
0.047305679
10
th
Lowest
Optimum Moisture
Pilar D. Galima
-0.171787098
0.073905186
14
th
Lowest
Optimum Moisture
Poblacion
North
-0.340126693
-0.298433425
4
th
Lowest
Dry Soil
Poblacion
South
-0.744469845
-0.620635318
2
nd
Lowest
Dry Soil
Quezon
-0.218476355
0.029448271
7
th
Lowest
Optimum Moisture
Quirino
-0.241473928
-0.18106429
6
th
Lowest
Optimum Moisture
Roxas
-0.222969472
0.047443677
11
th
Lowest
Optimum Moisture
San Juan
-0.152612522
0.091206992
15
th
Lowest
Optimum Moisture
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Generated Soil Moisture Map for year 2020 and 2025
Figure 3. Soil Moisture Map of Solano, Nueva Vizcaya for the year 2020
San Luis
-0.152640551
0.055470048
12
th
Lowest
Optimum Moisture
Tucal
-0.171593085
0.103613814
17
th
Lowest
Optimum Moisture
Uddiawan
-0.147683561
0.143109305
22
nd
Lowest
Optimum Moisture
Wacal
-0.184858501
0.068659498
13
th
Lowest
Optimum Moisture
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Figure 4. Soil Moisture Map of Solano, Nueva Vizcaya for the year 2025
DISCUSSION
Table 1 is the soil moisture classification table which defines the ranges for categorizing soil moisture levels.
Dry soil is classified as having soil moisture values from -1 up to -0.2. Optimum moisture is defined by soil
moisture values ranging from -0.2 to 0.4. Wet soil is characterized by soil moisture values spanning from 0.4 to
Table 2 shows the soil moisture values and classification of Solano for the years 2020 and 2025. In 2020, the
minimum soil moisture value for the whole municipality of Solano is -1, while the maximum reaches
0.702479362. The mean soil moisture value for this year is -0.119330379. Considering the soil moisture
classification table, this mean value falls within the Optimum Moisture range.
For 2025, the minimum soil moisture value for the whole municipality of Solano is -0.695321841, and the
maximum is 0.639916241. The mean soil moisture value for 2025 is 0.193653007. Referencing from the soil
moisture classification table, this mean value falls within the Optimum Moisture range.
Table 2 shows the variations of soil moisture levels in Solano, Nueva Vizcaya from 2020 to 2025 which reveals
notable changes in minimum and mean values, although the overall classification remains within the "Optimum
Moisture" category for both years.
By 2025, the minimum soil moisture level increased by 0.304678159, the maximum decreased by 0.062563121,
and the mean soil moisture significantly rose by 0.312983386.
The shift in mean soil moisture from -0.119330379 in 2020 to 0.193653007 in 2025 indicates a general increase
in soil moisture levels across the municipality. Despite these changes, both years fall under the "Optimum
Moisture" classification, which is defined by soil moisture values ranging from -0.2 to 0.4
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Table 3 shows the soil moisture data for the year 2020, categorized by barangays within the whole municipality
of Solano. The data includes minimum, maximum, and mean soil moisture values, along with a soil moisture
classification and rank for each barangay.
Figure 3 and Figure 4 represent the soil moisture map for the years 2020 and 2025. The analysis of soil moisture
levels in the municipality of Solano, Nueva Vizcaya, reveals a dynamic shift in moisture conditions across its
barangays and at the municipal level between 2020 and 2025. In 2020, the distribution of soil moisture among
barangays exhibited considerable diversity. Some barangays, such as Dadap, Poblacion South, Bangar, and
Poblacion North, were classified as dry soil, indicating relatively low moisture content, with Dadap recording
the lowest mean soil moisture of -0.652269548 and minimum values reaching -0.776470637. The majority of
barangays, however, fell into the optimum moisture category, suggesting generally favorable conditions for plant
growth, although mean soil moisture levels within this category varied from 0.029448271 in Quezon to
0.143109305 in Uddiawan, reflecting a spectrum of water availability. The wide ranges in minimum and
maximum soil moisture values within individual barangays also point to potential temporal or spatial variability.
By 2025, the soil moisture profile in Solano demonstrated a general trend towards increased moisture retention
in many areas. The dry soil classification was confined to only Poblacion North and Poblacion South, with
Poblacion South having the lowest mean soil moisture at -0.621713551 and a minimum of -0.695321841. Most
barangays continued to be classified as optimum moisture, but the mean soil moisture values within this category
generally increased, with Concepcion recording the highest mean soil moisture at 0.281513396.
CONCLUSION
This study aimed to map and compare soil moisture levels in Solano, Nueva Vizcaya, for 2020 and 2025 using
Sentinel-2 spectral bands and GIS techniques. Soil moisture, a critical parameter in various scientific and
engineering disciplines, including agriculture, hydrology, and climate science, was assessed using the
Normalized Difference Moisture Index (NDMI), calculated from Sentinel-2's Band 8A (Near Infrared) and Band
11 (Shortwave Infrared). The methodology involved data preprocessing using the Sentinel-2 Copernicus website
and thematic map creation in ArcGIS 10.8, following the conceptual framework of Input-Process-Output.
The findings revealed variations in soil moisture across Solano between 2020 and 2025. In 2020, the
municipality's mean soil moisture was -0.119330379, ranging from -1 to 0.702479362, classified as optimum
moisture. By 2025, the mean soil moisture increased to 0.193653007 having a minimum of -0.695321841 and a
maximum of 0.639916241, still within the optimum moisture range. Barangay-level analysis showed variations,
in 2020, barangays like Dadap had dry soil with a mean of -0.652269548, while in 2025, the dry soil classification
was less prevalent.
These results indicate a general increasing trend in soil moisture in Solano from 2020 to 2025, highlighting the
effectiveness of Sentinel-2 and GIS in monitoring soil moisture dynamics. These align with the broader
understanding of soil moisture dynamics and the capabilities of remote sensing. Soil moisture is recognized as a
key factor influencing agricultural productivity, hydrological processes, and climate patterns (Jackson & Hsu,
2004). Remote sensing techniques, particularly those employing Sentinel-2 data, have been demonstrated to be
effective in monitoring soil moisture over large areas, providing valuable data for environmental monitoring and
resource management (Rizzi, 2022). GIS tools play a crucial role in processing and analyzing remote sensing
data to generate spatial representations of soil moisture, enabling informed decision-making.
The findings of this study are valuable for stakeholders like the DENR and LGUs for informed decision-making
in agriculture, water management, and land use planning in the Solano municipality.
ACKNOWLEDGEMENT
The researchers extend their sincere gratitude to Copernicus Open Access Hub for the free access of Sentinel-2
imagery.
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