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In the supervised classification method, the use of the Maximum likelihood algorithm shall classify based on the sample set provided by the user based on their field knowle
shall be used for reference and understanding on the distribution of pixels. The “The classification result by the unsupervised classification method classification result divided into four classes of land cover including agricultural land, construction area, arid land and water areas determined in the research area, In the research of Li etal (2003) “Research of the change of cover in the Tarim basin ‘of China in the period of 1964 and 2000”, The author has used Landsat ETM image for the year 2000 Corona Panchromatic image for the year 1964. Using the method ‘of post-classification convulsion discovery, the author noticed a change in the area of reclaimed land from water and soil, the death of an old primeval forest surrounding ‘Tarim River and also the change in the salinity
In the research “Analysis of Urban Sprawl Pattern in Tiruchirappalli City Using Applications of Remote Sensing and GIS” (Nisha Radhakrishnan Satish Kumar Eerni -Sathees Kumar, 2013). The author used ASTER image with high resolution, collected from the national remote sensing center. Images after processing shall go through land cover classification via the ERDAS IMAGINE 9.1 software. In this research the author used the supervised classification method, and used the ‘Maximum likelihood Class
types of land cover which are construction soil, vegetation, moist soil, vacant land determined in the research area,
+ algorithm, The classification result divided into S
cover changes in Vietnam
‘Currently there have been many research works on the convulsion of land cover with many different viewpoints, of which there are works that focus on argumentative research analysis, while others focus on methods of finding convulsion and there are works that combine both: convulsion discovery technique, result assessment and argument supplementation,
‘The topic “Research of convulsion of several forms of land use in the peri-urban areas of Tu Liem district Hanoi city on the basis of remote sensing and GIS technology application” of author Nguyen Thi Thuy Hang has solved problems such as extraction of information on convulsion of land use from multispectral and multi
and time remote sensing data through several methods of digital image analysis
</div><span class="text_page_counter">Trang 16</span><div class="page_container" data-page="16">processing, integrating remote sensing data analysis results with other data to assess the correlation between convulsion of land use and socioeconomic phenomena.
‘The author group Nhu Thi Xuan, Dinh Thi Bao Hoa, Nguyen Thi Thuy Hang with the article “Assessment of land use convulsion of Thanh Tri district, Hanoi city in the period of 1994 - 2003 on the basis of remote sensing method combined with GIS” has analyzed, assessed the convulsion of land use in the area of Thanh Tri. This is also one of the areas largely affected by the urbanization,
In addition to using remote sensing data in the research of convulsion, author Hoang ‘Thi Thanh Huong in the topic “Research of convulsion of land use in Long Bien distr . Hanoi city during urbanization” has combined remote sensing material with the spatial analysis of the geo information system. The topic pilots the new classification method of classification by subject, method of performance on remote sensing data with very high resolution (VHR). In addition, spatial analysis is used in GIS to compare classification results with the socioeconomic data to see the interaction between them. The result shows that the remot snsing image with high spatial resolution can meet the requirements of accuracy of urban areas with fragmentation as in Vietnam.
In the topic “Establishment of vegetation map on the basis of remote sensing image analysis, processing” at the area of Tua Chua ~ Lai Chau (Hoang Xuan Thanh, 2006), the author used the supervised classification method for the Landsat image data of 2006 to classify 7 different vegetation classes with the Kapa index =0:7
In the topic “Application of remote sensing in monitoring the urban land convulsion
classification method was used to divide into 5 classes of subject. The most noteworthy point of this topic is the combined use of various remote sensing images such as Landsat (1992, 2000) and SPOT (2005) to bring forth the interpreted results, while also have a comparison on the accuracy, detail between the image types. With a Kappa index of =0,9, the SPOT image data has the post-classification accuracy higher than compared to Landsat (Kapa~0.7),
In the research “Application of remote sensing and GIS in establishing the land cover map of the area of Chan May, Phu Loc district, Thua Thien Hue province” (Nguyen Huy Anh, Dinh Thanh Kien, 2012), the author has used the most approximate classification method for the Landsat TM image data at a resolution of
</div><span class="text_page_counter">Trang 17</span><div class="page_container" data-page="17">10m, combined with field sampling to divide into 13 types of cover with relatively high accuracy
In the research “Usage of MODIS satellite image material in research of crop season, establishment of status quo and convulsion map of the Red River delta cover in the period of 2008 -2010" (Vu Huu Long, Pham Khanh Chi, Tran Hung, 2011), the author used supervised classification with the most approximate classification algorithm. The topic classfied 9 types of cover with Kapa index ~0,9. To assess the accuracy, the author used a combination of the survey sample data, field investigation and the status quo map of Land use of the most recent year
In the topic “Research of the impact of shifting agricultural land to non-agricultural land in the vicinity of Hue city, period of 2006 - 2010” (Nguyen Thi Phuong Anh et al, 2012), the author assessed the impact of the shift of agricultural land to non-agricultural land on the economic structure, social life and bring out viable solutions,
with the pilot research area being Kim Long ward. In this topic, the author only used
methods of synth
is, analysis, comparison, contrasting, and statistics of data to we data is extracted via tables, without visual output by system of
In the topic “Research of change of forest vegetation at the Bach Ma national garden, ‘Thua Thien Hue province” (Dang Ngoc Quoc Hung, 2009), the author built forest vegetation maps of the years 1989, 2001, 2004, 2007 by supervised method of
remote se ing image interpretation to extract information from satellite images Erdas software was used to interpret satellite images. The change of the forest
vegetation in the periods 1989-2001, 2001-2004, 2004-2007 was analyzed and
assessed by method of stacking and analysis by Arcview 3.2 software,
he application of remote sensi in monitoring the status of land use, although popular in the world, is still not widely applied in Vietnam. This may show that, the capability of remote sensing in status monitoring is very good but the performance of this task is still difficult, especially for small areas,
1.3. Approach of the research.
of land cover on the surface of the research area, combined with field survey and ‘other materials determining the status of land use
</div><span class="text_page_counter">Trang 18</span><div class="page_container" data-page="18"><small>and cover changemap 1999-2015,</small>
<small>Fvaluaiag theresus of and coverng</small>
Figure I. 1. Overview of the research
‘The GIS geographical information system is used to analyze, assess the convulsion of land resources.
area adhers to the following procedure
were used to analyze and establish the land cover map of 2 periods. The methods of remote sensing image analysis are very diverse. Some of the methods of image analysis can be Tisted such as manual threshold, unsupervised classification, supervised classification, Fuzzy classification or Mixing models but the two popular methods for classifying land cover currently is the unsupervised classification and supervised classification.
</div><span class="text_page_counter">Trang 19</span><div class="page_container" data-page="19">Each method of classification uses certain algorithms. The algorithms have limitation and application in different situations (Shrestha and Alfted, 2001). The
Likelihood (Richards, 1994). Among these, the Maximum Likelihoood algorithm is used the most by classifiers in works of land cover research (Keuchel et al, 2003 Shrestha and Alfred, 2001; Swain and Davis, 1978; Este etal, 1983; Schowengerdi,
1983; Sabins, 1986; Lillesand and Kiefer, 2000; Jensen, 1996). The Minimum Distance algorithm is often applied in the unsupervised classification method, while the two algorithms Maximum Likelihood and Parallelepiped are usually applied in
highlight the vegetation factor such as the vegetation index analysis method ~ NDVI
Maximum Likelihood algorithm to analyze the land cover of 2 periods on the research area,
“The calculation of land cover changes of two periods is done by the CROSSTAB tool (Cross-Classification) in the IDRISI 17 software. This method is the popular
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</div><span class="text_page_counter">Trang 20</span><div class="page_container" data-page="20">approach to calculation of land cover changes in land cover researches around the world,
1.3.1. The remote sensing is used for monitoring land cover changes
Remote sensing is a science of technology that helps to identify, measure or analyze the properties of objects or phenomena from a distance without direct contact with the abject.
different ways, known as spectral characteristics. These characteristics conta important information that allows the grouping of natural formations into objects of the same spectral reflectance. This is useful for the interpretation of satellite imagery so the spectral reflectance characteristics of natural objects play a very important role in exploiting and applying effectively the collected information,
Spectral reflectance properties of natural objects depend on many factors such as lighting conditions, aunospheric environment and object surface, especially the objects themselves (moisture, surface roughness, vegetation, humus, surface structure, ete.). Different objects will have ability to reflect different spectra, with ceach object, the reflecting and re-absorbing varies by wavelength. The remote sensing method relies primarily on this principle to identify and detect objects and
objects will help professionals select image processing methods to get optimal
basis to analyze and research of the properties of the object and proceed to classify them, The following is spectral reflective characteristics of some of the main natural
</div><span class="text_page_counter">Trang 21</span><div class="page_container" data-page="21">Solar radiation on the leaf surface, in the red and blue regions is absorbed by the chlorophyll for photosynthesis, in the green and infrared regions will be reflected when exposed too much chlorophyll of leaves (when plants are healthy), When plants are weak, chlorophyll decreases, the ability to reflect the red wave predominates, so leaves are yellow (green - red combination) or red in cold weather. ‘The difference in spectral reflective characteristics of plants depends on the internal and external constituents of the plant (chlorophyll content, the structure of the dermis, the composition and structure of the epidermis, the morphology of the
(growth conditions, lighting conditions, weather, geographical location, etc.) However, the spectral reflective characteristics of the vegetation cover still have the following common features: Reflected near the near-hip zone (2> 0.720qim), strongly absorbed in the red zone (1 = 0.680 - 0.270 jum).
Reflective spectral characteristics of water
‘The spectral reflectance of water also varies by the wavelength of the incoming radiation and the composition of materials in water. Water only reflects strongly in the blue wave zone and weakens when it reaches the green zones, and is destroyed at the end of the red strip. It also depends on the surface and state of the water.
Most of the sun's radiation energy is absorbed by water for the process of raising water temperature, The reflected energy of water consists of the energy reflected on the surface and the energy reflected afler scatterred with suspended materials in water. Therefore, the reflex energy of different types of water is very different,
and decreases by increasing wavelength. Solar radiation is almost completely absorbed in infrared and near infrared waves. The turbid water is stronger than the clear water in relfection, especially in the red zone due to the scattering effects of suspended materials. The use of photographs in long wave channels allows us to interpret water objects. For example, the waterfronts will be easily interpreted on infrared and near infrared channel.
‘The characteristic curve of the spectral reflectance of the terrestrial overlap gradually increases from the ullraviolet zone to infrared zone in a monotonous manner, with Tess obvious maxima and minima, The main reason is that the elements of the soil
"
</div><span class="text_page_counter">Trang 22</span><div class="page_container" data-page="22">are complex and not as clear as in plants. Spectral reflectance depends mainly on the physical and chemical nature of the soil, organic content, humidity, structure (sand, powder and clay fraction), state, surface and mechanical components of the soil. This causes the curve to fluctuate around an average value. However, the general rule is that the spectral value of the soil increases toward the longer wavelength
Reflective spectral characteristics of rock
Rock has mass and dry structure with the same spectral reflectance curve similar to soil but the absolute value is usually higher. However, as for soil, the fluctuation of the reflectance value depends on many factors of the rock: water level, structure, ‘composition, mineral composition, surface condition, ete
In short, reflection spectrum is the most important information that remote sensing has obtained about the objects. Based on the reflection spectral characteristics (intensity, curvature in different wave bands), itis possible to analyze, compare and identify objects on the surface. Specal information is the first information, which is the premise for image analysis methods in remote sensing, pecially digital
Different objects within the same group of objects will have the same general spectral-reflection curve type, but they will be different in terms of small details on the curve or varying in magnitude of reflection value, When the nature of the object ‘changes, the spectral curve is also varied. Based on these characteristics, there are signs of interpretation for objects on satellite images as follows
<small>- Photo elements:</small>
+ Brightness (fone): The sum of light reflected by the object's surface, which is a very important interpretative sign for object identification.
+ Texture: texture is interpreted as the number of repetitions of tone changes caused by the aggregation of many distinct characteristics of individuals. For example, the fine structure typical of loose sediment, the coarse structure typical of magmatic rocks, the strip structure characteristic of metamorphic sedimentary rocks. Accordingly, it is possible to distinguish between different rocks and their relative
+ Pattern: A very important element that represents the arrangement of objects according to a certain law in space. A particular type of terrain would inelude the
</div><span class="text_page_counter">Trang 23</span><div class="page_container" data-page="23">arrangement in accordance with a specific rule of natural objects which are ‘components of such terrain forms, For example, concentrated urban areas of houses, streets, and trees that make up a distinctive pattern of urban structure, Rice paddies have distinctive patterns that differ from orchards,
+ Shape: The external characteri typical for each object, the external image of the object. Shape is the first factor that helps the analysts distinguish between different objects, For example, the horseshoe lake is a narrow river, bright broom type is the coastal sand dunes.
+ Size: The size of an object is determined by the ratio of imagery and size measured ‘on the image. Based on this information we can also di inguish the objects on the
+ Shadow: the obscured part, no sunlight or light from active source, so there is no light reflected back to the receiver. Shadows are usually represented by black tone on black and white and dark to bla
on color image. The shadow can reflect on the tht of the object. Shadow is an important element that creates the characteristic about the object is not available or very little, so the amount of information needs to bè added in this zone.
+ Site: site is also a very important clement to distinguish objects, With the s sign, but in different sites it may be different objects. For example, the mudflats ‘cannot be found on the mountain slope, although some of the characteristics of the image look very much li is sign. The mudflats are distributed only on both sides
are the discharge cones, sliding zones or shifting cultivation areas.
interpreter to distinguish many objects with similar color tone characte
black and white images. The common color combinations used in LANDSAT and
ties on
SPOT images are blue, green and red representing the basic elements of pink to reddish-green plants, light to dark green water, dark red to dark brown mangrove forests, pink to yellow bare land with winter crops, ete.
In addition to the above three fake-color combinations, we can create many other different fake color combinations using optical method (using color filters) or digital image processing techniques. Therefore, when interpreting the objects on fake color
B
</div><span class="text_page_counter">Trang 24</span><div class="page_container" data-page="24">images, there must be early orientations on fake color combinations, thus avoiding confusion.
- Geotechnical elements
Elements of topography, vegetation, land use status, river network, cracks system and linear elements, combinatorial of interpretation elements, Following are some <small>interpretive signs:</small>
Table 1. 1 Some interpretation signs on the fake color combination of SPOT satellite images
1 | Cities Blue (dark or light, even white depending on the density of the building works)
‘Traffic (road, Dark blue or grey.
S5 | Perennials Red — pink
Source: Snidy on rational use of suburban land in Thanh Tri district, Hanoi with the support of remote sensing and geographic information system - Dinh Thi Bao Hoa, 2007.
So in visual judgments, itis needed to capture and distinguish between interpretative signs, the work requires the interpreter to have a good knowledge in order to
can be released.
1.3.2 GIS spatial analysis is used for evaluation of land cover changes ‘Ther © are many concepts about GIS but generally they are in two directions:
<small>= The concept of GIS as a map database controlled by computer graphics techniques</small> with the functions of importing, organizing, displaying, querying the map information stored in the database.
</div><span class="text_page_counter">Trang 25</span><div class="page_container" data-page="25">- The concept of GIS as a geographic information system including functions of input, analysis and display, and able to modelization the information layers ‘organized in a database to create thematic maps.
Regardless of GIS's concepts, it both has to meet the requirements of a four-part information system:
1, Computers and peripherals capable of performing software input, output and
2. A software capable of entering, storing, adjusting, updating and organizing spatial information and attribute information, analyzing, transforming information in a database, displaying and presenting information in different forms, with different 3. With a database containing spatial information (geographic information) and attribute information, organized according to a specific specialized intention
4. User ‘with specialized expert knowledge.
In the land cover change study, GIS plays an important role in gathering and analyzing database. It is aimed to synthesize, systematize and unify the data sources for monitoring and evaluating land cover variation.
“The strength of a GIS is expressed through spatial analysis. Spatial analysis is often used to generate additional geographic information using existing information or developing spatial structures or relationships between geographic information. In the
Creating additional geographic information overlapping the data layer or creating a
are overlapped by an algebraic or logical operation to obtain a new data, Buffering is
determining the area within a certain radius as compared to an object or point.
‘Typically, the length of the buffer zone radius is determined by the effect of the point ‘or path to the surrounding area,
Linking Technique: Linking multiple spatial analysis techniques together to get the results needed.
In addition, to search for data that satisfies a set condition, the author also use the spatial query function of GIS, There are two types of spatial query that are attribute data query (it means to find a spatial distribution or a region that satisfies certain
1s
</div><span class="text_page_counter">Trang 26</span><div class="page_container" data-page="26">attribute conditions) and geographic data query (search all data satisfying a given ‘geographical condition such as position, shape or intersection, etc.)
Searching and analyzing data depend on the ability to link these two data types. The ‘greater the linking capacity, the better the search and analysis of data. Users can access table data through the map or can create maps through the table data, To access and display this data, the computer needs to store both tabular and graphical data in an organized and searchable format
</div><span class="text_page_counter">Trang 27</span><div class="page_container" data-page="27">2.1, Overview of study area
2.1.1. Natural and socio-economic conditions
Son La is a mountainous province in Northwest Vietnam, with an area of 14,12 ket, accounting for 4.27% of Vietnam's total area, ranking third among 63 provinces
north; Phu Tho and Hoa Binh to the east; bordered Dien Bien province in the west bordered Thanh Hoa province and Huaphanh province (Laos) in the south; and
Luangprabang Province (Laos) in the southwest, Son La has a national boundary of
administrative units (I city, 11 districts) with 12 ethnic groups.
Son La has subtropical moist montane climate, cold dry non-tropical winter, hot and humid summer, heavy rain, Due to the deep and strong geographical divided terrain, many sub-climates are formed, allowing for the development of a rich agro-forestry
along the Da River is suitable for tropical evergreen forests, Statistics show that the
an increase of 0.5 ° C - 06° C, the average annual temperature in Son La is at 21.1 ° ©, Yen Chau 23 ° C; Average annual rainfall tends to decrease (city is currently at 1,402 mm, Moc Chau 1,563 mm); Average annual humidity also declines. The <rought in winter, the hot and dry west wind in the last months of the dry season and at the beginning of rainy season (March - April), are the factors affecting the agricultural production of the province. Salt fog, hail, flash floods are unfavorable
Son La is still one of the poor provinces of the country. There are 11 districts and 1 city in the whole province, in which there are 5 poor districts under the Government's program for Rapid and Sustainable Poverty Reduction (Program 30) In recent years, the introduction of Son La hydropower projects has contributed significantly to the overall change of infrastructure, creating a motive force for Son
0
</div><span class="text_page_counter">Trang 28</span><div class="page_container" data-page="28">La province to develop. In mountainous districts, agriculture is still their strength With the propaganda of knowledge, farmers have boldly renewed crops and cultivation methods, bringing productivity increased 4-5 times.
According to the results of collecting and compiling documents of the Northern Geological Mapping Division in 2013, the forest distribution in Son La province accounts for 45.49% of the provincial area in 2011, while the area of bare soil accounts for 33.78%. Specifically, the area of Son La province has the following
- Special-use forest - protection forest: occupying 15% of Son La province. forest type with green state all year round, leaves are often broad-leaf, small to medium leaf size. The soil in the Forest is usually moist, thick, yellow or brown, Due to the high deforestation at present, this forest type is mainly secondary forest, the soil is strong degraded, secondary vegetation is no longer wood but converted into bamboo forest.
- Plantation forest - zonation forest (production forest): occupying 22.59% of the
area of Son La province, is a forest type with many layers, thick trees, closed ‘canopy, the highest plant only 20-30m. Few additional trees and parasites. The soil is thin and dry. Some areas are further degraded, becoming deciduous for vegetation cover is bush with sim, mua, sam and finally hay.
- Shrub - grassland: occupying 8% of the (otal area of Son La province, including mangroves, scrublands and grasslands. In this type of forest, thick and scattered
woods are degraded by human impact.
Table 2. 1 Distribution of vegetation cover and current land use status in 20111
No, | T9Pe of lind cover Distributed area Area proportion <small>cover (km2) 6)</small> 5 [River-take 36612494
6 [Bare soil 46279892 33.78)
- Rice - crops: occupying 15.8% of the area of Son La province, this is a human ecological system created and maintained by humans for food and other essential
usually has only one species, intercropping a maximum of 2-3 species (maize-beans, sh, long-term industrial crops, vegetables) leading unbalanced nutrient use in
the soil, In case of extensive cultivation, the productivity is not high compared to the productivity of natural ecological systems. Morevover, this ecosystem is very fragile, vulnerable to natural disasters, If intensive, it will degrade the environment, cause soil erosion and fading.
- Bare soil, rivers and lakes, and residential areas: accounting for about 38.6% of the total area of Son La province. In which vacant and bare land is too large, so it is
in a reasonable manner, contributing to minimize the damage caused by the
2.2, Data collection and analysis 2.2.1. Remote sensing data
Within the scope of the study, the author has collected Landsat 7 and Landsat 8 image data for the study area from 1992 to 2015, with a resolution of 30m taken
128/46, The details are shown in Table 3
</div><span class="text_page_counter">Trang 30</span><div class="page_container" data-page="30">Table 2. 2 Remote sensing image data
Son La province is covered by four image scenes: PI28R45, PI28R46, P]27R45 and PI26R46. But the scene of P128R45 occupies most of the area (> 90%), so when 4 Mosaics are mixed together, the Landsat8 and Landsat7 images of Son La province ‘will be taken time of fly shooting as time of P128 / R45 scene.
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</div><span class="text_page_counter">Trang 31</span><div class="page_container" data-page="31">igure 2. 1 Scene P128-R45 covers 90% area of Son La province 2.2.2. Land use status
Son La province has a total area of 1.405.500 ha. The results of the survey on the soil mapping in scale of 1 / 100,000 of Son La province show that:
Son La is a mountainous province with strong divided terrain, there are 85% (about
climate features, much rain, seasonal focus. Most of the area of annual trees are cultivated on sloping land, strongly eroded soil. This is a pressing problem in the use such as water of land, damaging land ssources and affecting other resoure:
resources, vegetation and ecological environment,
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</div><span class="text_page_counter">Trang 32</span><div class="page_container" data-page="32">Table 2. 3 Land use status of Son La province in 2005 as follows:
Total natural area 1.405.500 100,00 1__| Agricultural land group 672.485 4185
112 | Land of kaingin 123.084 7148
1.2 _| Mixed garden soil 6933 3.61 13 _| Land for perennial crops 2.584 177 1.4 _| Land for grass planting for livestock 1832 0.96 15 _| Land with water surface for aquaculture 1624 085 2 |Forestryland 480.657 7174 2.1 | Land with natural forest 439.592 91.46 2.1.1 | Forest land for production 50.297 nas 2.1.2 | Protective forest land 322.149 73.28 2.1.3. | Special-use forest land 67.146 1528 2.2 _| Land with planted forest 41.087 854 2.2.1. | Forest land for production 8364 2038 2.2.2 | Protective forest land 32646 79/53 2.2.3. | Special-use forest land 37 009 2.3 _| Land for nursing seedlings 18 0
1 _| Residential land 6.033, 19.93 Lt | Rural land 438 7.30
2
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