Prioritization of watershed has picked up significance in watershed management. Morphometic analysis is been commonly applied to prioritize the watershed. The present study makes an effort to organize subwatersheds dependent on morphometric characteristics using GIS techniques in Part of Cauvery region. There are twenty three Subwatersheds under this. Various morphometric parameters namely Bifurcation ratio(Rb), Drainage density(Dd), Stream frequency(Ns), Texture ratio(T), Form factor(Rf), Circularity ratio(Rc), Elongation Ratio(Re), length of overland flow, shape factor(Bs), drainage texture, compactness ratio (Cc) has been determined for each subwatershed and allotted position on premise of relationship as to arrive at a computed value for final ranking of subwatershed.
What is prioritization?
Prioritization is done to select the area of interest.
Prioritization is a process of identifying areas of main concern based on single or many parameters
Selection of one or few watersheds out of many watersheds by using predefined set of criteria.
Morphometric Studies of Fourth order Sub-Basins (FOSB’s) in North Bangalore M...Dr Ramesh Dikpal
The quantitative analysis of drainage system is an important aspect of characterization of watersheds. Using watershed as a basic unit in morphometric analysis is the most logical choice because all hydrologic and geomorphic processes occur within the watershed. The North Bangalore Metropolitan Region is constitutes a part of North Pennar, South Pennar and Cauvery Basins has been selected for the case illustration. Geo-informatics module consists of GIS mapping for location map, drainage map, surface water body map, sub-basin map etc are generated. Morphometric module consists of morphometric analysis for several drainage basin parameters include stream order, stream length, bifurcation ratio, drainage density, drainage frequency, form factor, elongation ratio, circularity ratio, texture ratio, length of overland flow and constant of channel maintenance are also calculated. An attempt has been made to utilize the interpretation capabilities of GIS to find out the relationship between the morphometric parameters at sub basin level.
The Effect of Geometry Parameters and Flow Characteristics on Erosion and Sed...Dr. Amarjeet Singh
One of the most critical problems in the river
engineering field is scouring, sedimentation and morphology
of a river bed. In this paper, a finite volume method
FORTRAN code is provided and used. The code is able to
model the sedimentation. The flow and sediment were
modeled at the interception of the two channels. It is applied
an experimental model to evaluate the results. Regarding the
numerical model, the effects of geometry parameters such as
proportion of secondary channel to main channel width and
intersection angle and also hydraulic conditionals like
secondary to main channel discharge ratio and inlet flow
Froude number were studied on bed topographical and flow
pattern. The numerical results show that the maximum
height of bed increased to 32 percent as the discharge ratio
reaches to 51 percent, on average. It is observed that the
maximum height of sedimentation decreases by declining in
main channel to secondary channel Froude number ratio. On
the assessment of the channel width, velocity and final bed
height variations have changed by given trend, in all the
ratios. Also, increasing in the intersection angle accompanied
by decreasing in flow velocity variations along the channel.
The pattern of velocity and topographical bed variations are
also constant in any studied angles.
Groundwater models are simplified representation of large and real hydrogeologic systems like river basins or watersheds. GWM is attempted to analyse the mechanisms which control the occurrence and movement of groundwater and to evaluate the policies, actions and designs which may affect the systems. These models are less complex prototypes of complex hydrogeologic systems developed using spatially varying aquifer parameters, hydrologic properties, geologic boundary conditions and positions of withdrawal wells or recharging structures. These are designed to compute how pumping or recharge might affect the local or regional groundwater levels.
- Morphometric analysis of the Watershed is considered to be the most satisfactory method because it enables in
understanding of the relationship of various aspects within a drainage basin. In the present study two mini watersheds in Raichur city
have been considered Mini-watershed 1 with an area of 519.32 km2 with highest order stream of 6 it flows through north of city and it
joins the streams of Krishna, Mini –Watershed 2 with an area of 360.97 km2 with highest order stream of 5 it flows through south of
city and joins Tungabhadra streams. The values of Stream frequency is 1.07 and 1.03, Form factor 0.35and 0.53, Shape factor 2.84 and
1.90, Elongation Ratio 0.67 and 0.82, Circularity Ratio 0.27 and 0.42, Drainage density 1.26 and 1.30, Length of overland flow 0.40 and
0.38 for Mini-watershed 1 and Mini-watershed 2 respectively
What is prioritization?
Prioritization is done to select the area of interest.
Prioritization is a process of identifying areas of main concern based on single or many parameters
Selection of one or few watersheds out of many watersheds by using predefined set of criteria.
Morphometric Studies of Fourth order Sub-Basins (FOSB’s) in North Bangalore M...Dr Ramesh Dikpal
The quantitative analysis of drainage system is an important aspect of characterization of watersheds. Using watershed as a basic unit in morphometric analysis is the most logical choice because all hydrologic and geomorphic processes occur within the watershed. The North Bangalore Metropolitan Region is constitutes a part of North Pennar, South Pennar and Cauvery Basins has been selected for the case illustration. Geo-informatics module consists of GIS mapping for location map, drainage map, surface water body map, sub-basin map etc are generated. Morphometric module consists of morphometric analysis for several drainage basin parameters include stream order, stream length, bifurcation ratio, drainage density, drainage frequency, form factor, elongation ratio, circularity ratio, texture ratio, length of overland flow and constant of channel maintenance are also calculated. An attempt has been made to utilize the interpretation capabilities of GIS to find out the relationship between the morphometric parameters at sub basin level.
The Effect of Geometry Parameters and Flow Characteristics on Erosion and Sed...Dr. Amarjeet Singh
One of the most critical problems in the river
engineering field is scouring, sedimentation and morphology
of a river bed. In this paper, a finite volume method
FORTRAN code is provided and used. The code is able to
model the sedimentation. The flow and sediment were
modeled at the interception of the two channels. It is applied
an experimental model to evaluate the results. Regarding the
numerical model, the effects of geometry parameters such as
proportion of secondary channel to main channel width and
intersection angle and also hydraulic conditionals like
secondary to main channel discharge ratio and inlet flow
Froude number were studied on bed topographical and flow
pattern. The numerical results show that the maximum
height of bed increased to 32 percent as the discharge ratio
reaches to 51 percent, on average. It is observed that the
maximum height of sedimentation decreases by declining in
main channel to secondary channel Froude number ratio. On
the assessment of the channel width, velocity and final bed
height variations have changed by given trend, in all the
ratios. Also, increasing in the intersection angle accompanied
by decreasing in flow velocity variations along the channel.
The pattern of velocity and topographical bed variations are
also constant in any studied angles.
Groundwater models are simplified representation of large and real hydrogeologic systems like river basins or watersheds. GWM is attempted to analyse the mechanisms which control the occurrence and movement of groundwater and to evaluate the policies, actions and designs which may affect the systems. These models are less complex prototypes of complex hydrogeologic systems developed using spatially varying aquifer parameters, hydrologic properties, geologic boundary conditions and positions of withdrawal wells or recharging structures. These are designed to compute how pumping or recharge might affect the local or regional groundwater levels.
- Morphometric analysis of the Watershed is considered to be the most satisfactory method because it enables in
understanding of the relationship of various aspects within a drainage basin. In the present study two mini watersheds in Raichur city
have been considered Mini-watershed 1 with an area of 519.32 km2 with highest order stream of 6 it flows through north of city and it
joins the streams of Krishna, Mini –Watershed 2 with an area of 360.97 km2 with highest order stream of 5 it flows through south of
city and joins Tungabhadra streams. The values of Stream frequency is 1.07 and 1.03, Form factor 0.35and 0.53, Shape factor 2.84 and
1.90, Elongation Ratio 0.67 and 0.82, Circularity Ratio 0.27 and 0.42, Drainage density 1.26 and 1.30, Length of overland flow 0.40 and
0.38 for Mini-watershed 1 and Mini-watershed 2 respectively
Quantitative evaluation and analysis of morphometric parameters derived from ...AM Publications
GIS has become a key source to understand the hydrological conditions of watersheds for the last few decades. Arc Hydro tool of ArcGIS has been proven its role in the automated extraction of drainage network and morphometric analysis from DEMs. The delineation of drainage network can be done either manually from topographic sheets or derived from Digital Elevation Model (DEM) data by means of computational methods. In the present work, ASTER DEM has been incurred to extract drainage network with the aid of Arc hydro tool. The Vaishali River basin of Madhya Pradesh has been taken as the study area. This study has been done primarily based on a geo-spatial software ARC GIS in which ARC HYDRO a tool has been used extensively. The quantitative evaluation and analysis of about twenty morphometric parameters has been done based on the linear, areal and relief aspects. The analysis has revealed that the Vaishali River basin is a fifth order basin showing dendritic drainage pattern with drainage density of 0.40 per km and stream frequency of 0.08 per km2. Low drainage density indicates the basin has not been much affected by structural disturbances while drainage frequency and very coarse drainage texture specifies low relief and porous, permeable rocks beneath the ground surface. The form factor, circularity ratio and elongated ratio suggest the basin shape as elongated. The area has low to moderate relief and slopes displays moderate relief ratios. It is concluded that this technique is not only reduces time but also provides valuable results which are very helpful for watershed management studies.
Prioritization of watershed has picked up significance in watershed management. Morphometic analysis is been commonly applied to prioritize the watershed. In the present study two mini watersheds in Raichur city have been considered Mini-watershed 1 with an area of 519.32 km2 with highest order stream of 6 Mini -Watershed 2 with an area of 360.97 km2 with highest order stream of 5. There are Seven Subwatersheds in both the Mini-watersheds. Various morphometric parameters namely Bifurcation ratio(Rb), Drainage density(Dd), Stream frequency(Ns), Texture ratio(T), Form factor(Rf), Circularity ratio(Rc), Elongation Ratio(Re), length of overland flow, shape factor(Bs), compactness ratio (Cc) has been determined for each subwatershed and allotted position on premise of relationship as to arrive at a Compound value for final ranking of subwatershed. The morphometric parameters ranges between Rb (2.95-5.50), Dd (1.218-1.373), Ns (0.890-1.182), T (0.731-1.590), Rf (0.230-0.850), Rc (0.246-0.500), Re (0.55-1.04), Cc (1.40-1.83), Lof (0.364-0.411), and Bs (1.17-4.20). It is found that in Mini-watershed 1 50.87% of area falls under Very high Priority category 32.94% under high, 8.96% under medium and 7.23% under very low priority category and in Mini-watershed 2 20.34% of area falls under very high, 19.82% under high and 59.84% under medium priority category.
Quantitative evaluation and analysis of morphometric parameters derived from ...AM Publications
GIS has become a key source to understand the hydrological conditions of watersheds for the last few decades. Arc Hydro tool of ArcGIS has been proven its role in the automated extraction of drainage network and morphometric analysis from DEMs. The delineation of drainage network can be done either manually from topographic sheets or derived from Digital Elevation Model (DEM) data by means of computational methods. In the present work, ASTER DEM has been incurred to extract drainage network with the aid of Arc hydro tool. The Vaishali River basin of Madhya Pradesh has been taken as the study area. This study has been done primarily based on a geo-spatial software ARC GIS in which ARC HYDRO a tool has been used extensively. The quantitative evaluation and analysis of about twenty morphometric parameters has been done based on the linear, areal and relief aspects. The analysis has revealed that the Vaishali River basin is a fifth order basin showing dendritic drainage pattern with drainage density of 0.40 per km and stream frequency of 0.08 per km2. Low drainage density indicates the basin has not been much affected by structural disturbances while drainage frequency and very coarse drainage texture specifies low relief and porous, permeable rocks beneath the ground surface. The form factor, circularity ratio and elongated ratio suggest the basin shape as elongated. The area has low to moderate relief and slopes displays moderate relief ratios. It is concluded that this technique is not only reduces time but also provides valuable results which are very helpful for watershed management studies.
Prioritization of watershed has picked up significance in watershed management. Morphometic analysis is been commonly applied to prioritize the watershed. In the present study two mini watersheds in Raichur city have been considered Mini-watershed 1 with an area of 519.32 km2 with highest order stream of 6 Mini -Watershed 2 with an area of 360.97 km2 with highest order stream of 5. There are Seven Subwatersheds in both the Mini-watersheds. Various morphometric parameters namely Bifurcation ratio(Rb), Drainage density(Dd), Stream frequency(Ns), Texture ratio(T), Form factor(Rf), Circularity ratio(Rc), Elongation Ratio(Re), length of overland flow, shape factor(Bs), compactness ratio (Cc) has been determined for each subwatershed and allotted position on premise of relationship as to arrive at a Compound value for final ranking of subwatershed. The morphometric parameters ranges between Rb (2.95-5.50), Dd (1.218-1.373), Ns (0.890-1.182), T (0.731-1.590), Rf (0.230-0.850), Rc (0.246-0.500), Re (0.55-1.04), Cc (1.40-1.83), Lof (0.364-0.411), and Bs (1.17-4.20). It is found that in Mini-watershed 1 50.87% of area falls under Very high Priority category 32.94% under high, 8.96% under medium and 7.23% under very low priority category and in Mini-watershed 2 20.34% of area falls under very high, 19.82% under high and 59.84% under medium priority category.
MORPHOMETRIC ANALYSIS OF SUKE SUB-WATERSHED OF TAWA RESERVOIR CATCHMENT AREA ...Journal For Research
The study area covers 732.95 Km2 in suke sub-watershed of Tawa reservoir catchment area of Hoshangabad, Bhopal (M.P.). the drainage network of suke sub watershed and measurement of Linear, Aereal and Relief aspects of basin by digitized using remote sensing and GIS techniques. The drainage network shows that the terrain exhibits dendritic drainage pattern. Stream order ranges from one to sixth order. The drainage density in the area 2.06km/km.2 belong to moderate category.Stream frequency in the area 2.82 and texture ratio 4.08 is range to belong moderate condition. The form factor indicate the sub watershed are less elongated in shape. The high value of circulatory ration the sub watershed is characterize by high to moderate relief and drainage system structurally controlled but the study area Rc is less than .50 indicating they are less elongated in shape.
IJRET : International Journal of Research in Engineering and Technology is an international peer reviewed, online journal published by eSAT Publishing House for the enhancement of research in various disciplines of Engineering and Technology. The aim and scope of the journal is to provide an academic medium and an important reference for the advancement and dissemination of research results that support high-level learning, teaching and research in the fields of Engineering and Technology. We bring together Scientists, Academician, Field Engineers, Scholars and Students of related fields of Engineering and Technology
Estimation of morphometric parameters and runoff using rs & gis techniqueseSAT Journals
Abstract
Land and water are the two vital natural resources, the optimal management of these resources with minimum adverse environmental
impact are essential not only for sustainable development but also for human survival. Satellite remote sensing with geographic
information system has a pragmatic approach to map and generate spatial input layers of predicting response behavior and yield of
watershed. Hence, in the present study an attempt has been made to understand the hydrological process of the catchment at the
watershed level by drawing the inferences from moprhometric analysis and runoff. The study area chosen for the present study is
Yagachi catchment situated in Chickamaglur and Hassan district lies geographically at a longitude 75⁰52’08.77”E and
13⁰10’50.77”N latitude. It covers an area of 559.493 Sq.km. Morphometric analysis is carried out to estimate morphometric
parameters at Micro-watershed to understand the hydrological response of the catchment at the Micro-watershed level. Daily runoff
is estimated using USDA SCS curve number model for a period of 10 years from 2001 to 2010. The rainfall runoff relationship of the
study shows there is a positive correlation.
Keywords: morphometric analysis, runoff, remote sensing and GIS, SCS - method
Estimation of morphometric parameters and runoff using rs & gis techniqueseSAT Journals
Abstract
Land and water are the two vital natural resources, the optimal management of these resources with minimum adverse environmental
impact are essential not only for sustainable development but also for human survival. Satellite remote sensing with geographic
information system has a pragmatic approach to map and generate spatial input layers of predicting response behavior and yield of
watershed. Hence, in the present study an attempt has been made to understand the hydrological process of the catchment at the
watershed level by drawing the inferences from moprhometric analysis and runoff. The study area chosen for the present study is
Yagachi catchment situated in Chickamaglur and Hassan district lies geographically at a longitude 75⁰52’08.77”E and
13⁰10’50.77”N latitude. It covers an area of 559.493 Sq.km. Morphometric analysis is carried out to estimate morphometric
parameters at Micro-watershed to understand the hydrological response of the catchment at the Micro-watershed level. Daily runoff
is estimated using USDA SCS curve number model for a period of 10 years from 2001 to 2010. The rainfall runoff relationship of the
study shows there is a positive correlation.
Keywords: morphometric analysis, runoff, remote sensing and GIS, SCS - method
-
2018 GIS in Education: GIS Watershed Delineation and Morphometric Analysis of...GIS in the Rockies
GIS watershed delineation is an essential part of water resource management. With increasingly available high-resolution data, hydrologic modelling is often more economical than field delineations; however, sources of errors and degree of correctness are often underestimated or unknown (Li and Wong, 2010). Although there are studies analyzing morphometric properties for DEM-derived watersheds, there are very few that compare morphometric properties between different DEM resolutions. This study performs an ArcHydro delineation for three DEM datasets and analyze the morphometric properties of the watersheds to determine differences from spatial resolution and source DEM. The study area is within the upper Vltava River in the Czech Republic and hydrologically-corrected 30-meter NASA SRTM DEM, and a 5- and 2-meter DTM from the Czech Republic Land Survey Office were used for the delineation. Twenty-two morphometric properties of the extracted watersheds were analyzed, and an accuracy assessment was performed. Results show total area and shape of each watershed were similar, but drainage density, number of subwatersheds, and mean elevation varied. Additionally, total stream length and length ratio is lowest for the SRTM watershed, suggesting that increased point density decreases interpolation error and increases both terrain surface and drainage network variability. However, performance time should be considered, with Flow Direction taking 10-times longer for the 5G DEM than for the SRTM dataset. Furthermore, a cost-benefit analysis to determine the resolution needed for the expected outcome should be performed. Lastly, understanding differences in algorithms used to extract the watershed and river network is essential for GIS best practices.
Evaluation of Morphometric Parameters Derived from CartoDEM and Aster GDEM wi...Dr Ramesh Dikpal
From three different sources viz. survey of India topographic map (1:50,000), CartoDEM (10 mts) and Aster GDEM (30 mts) morphometric parameters are derived and evaluated. Manually digitized the drainage network from toposheets and extracted drainage network system from CartoDEM and Aster GDEM using ArcGIS 10.2 software. Basic, derived and shape parameters are considered for basin analysis. The mean bifurcation ratio of the given basin for CartoDEM & Aster GDEM are having nearby values and also indicates some sort of geological control, high stream frequency (Fs) is indicative of high relief and low infiltration capacity of the bedrock pointing towards the increase in stream population with respect to increase in drainage density, low drainage density (Dd) leads to coarse drainage texture, value of Lg for topographic, CartoDEM and Aster GDEM data indicating very fine texture & fine texture respectively. From the shape parameters the Kumudvathi watershed indicates it is sub-circular and elongated. The results from the high resolution data will have the nearby values and less of % variation, whereas in low resolution data % of variation is more and will not meet criteria.
Evaluation of morphometric parameters derived from Cartosat-1 DEM using remot...Dr Ramesh Dikpal
The quantitative analysis of drainage system is
an important aspect of characterization of watersheds.
Using watershed as a basin unit in morphometric analysis
is the most logical choice because all hydrological and
geomorphic processes occur within the watershed. The
Budigere Amanikere watershed a tributary of Dakshina
Pinakini River has been selected for case illustration.
Geoinformatics module consisting of ArcGIS 10.3v and
Cartosat-1 Digital Elevation Model (DEM) version 1 of
resolution 1 arc Sec (*32 m) data obtained from Bhuvan
is effectively used. Sheet and gully erosion are identified in
parts of the study area. Slope in the watershed indicating
moderate to least runoff and negligible soil loss condition.
Third and fourth-order sub-watershed analysis is carried
out. Mean bifurcation ratio (Rb) 3.6 specify there is no
dominant influence of geology and structures, low drainage
density (Dd) 1.12 and low stream frequency (Fs) 1.17
implies highly infiltration subsoil material and low runoff,
infiltration number (If)1.3 implies higher infiltration
capacity, coarse drainage texture (T) 3.40 shows high
permeable subsoil, length of overland flow (Lg) 0.45
indicates under very less structural disturbances, less runoff
conditions, constant of channel maintenance (C) 0.9 indicates
higher permeability of subsoil, elongation ratio (Re)
0.58, circularity ratio (Rc) 0.75 and form factor (Rf) 0.26
signifies sub-circular to more elongated basin with high
infiltration with low runoff. It was observed from the
hypsometric curves and hypsometric integral values of the
watershed along with their sub basins that the drainage
system is attaining a mature stage of geomorphic development.
Additionally, Hypsometric curve and hypsometric
integral value proves that the infiltration capacity is high as
well as runoff is low in the watershed. Thus, these mormometric
analyses can be used as an estimator of erosion
status of watersheds leading to prioritization for taking up
soil and water conservation measures.
landform is a natural or artificial feature of the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. The Study area located between Latitude 15º54′2′′ N to 16º16′19′′ N Latitude and 76º48′40′′ E to77º4′21′′ E Longitude. The study area covers an area of 466.02 km2, having maximum length of 36.5 km.The study of hypsometric properties of watershed using hypsometric integral (HI) and hypsometric curve retrieved in that, HI value is 0.51 and hence watershed falls under the Mature Stage
Suspended Sediment Rating Curve for Tigris River Upstream Al- Betera RegulatorIJRES Journal
In this study, suspended sediment rating curves for sediment concentration for a section of Tigris
River located upstream AL-Betera regulator, Maysan province. For this purpose. Also, for each observation, the
river discharge was measured using the ADCP . Abased previous years data have been benefiting from the
vicissitudes of time of study area and took the annual discharge rate for each year and then entered into the
equation for calculation of suspended sediment through draw the relationship between discharge and sediment
suspended ,noticed power link between data and a good agreement between the power relation and the observed
data were achieved depending on the value of correlation coefficient R.
Streamflow simulation using radar-based precipitation applied to the Illinois...Alireza Safari
This paper describes the application of a spatially distributed hydrological model WetSpa (Water and Energy Transfer between Soil, Plants and Atmosphere) using radar-based rainfall data provide by the United States Hydrology Laboratory of NOAA's National Weather Service for a distributed model intercomparison project. The model is applied to the
river basin above Tahlequah hydrometry station with 30-m spatial resolution and one hour time--step for a total simulation period of 6 years. Rainfall inputs are derived from radar. The distributed model parameters are based on an extensive database of watershed characteristics available for the region, including digital maps of DEM, soil type, and land use. The model is calibrated and validated on part of the river flow records. The simulated hydrograph shows a good correspondence with observation (Nash efficiency coeffiecient >80%, indicating that the model is able to simulate the relevant hydrologic processes in the basin accurately.
In an ecosystem, there is need to establish the quantity and quality of resources and their suitability for a certain range of land uses in order to assure its future productivity and sustainability of biodiversity. Texture, pH, salinity (EC), sodicity (ESP), slope, temperature and effective soil depth were recognized as factors affecting land suitability for wheat production in the study area. Rabia method was used to generate the final Wheat Crop Suitability Map. It was found that 50.68 percentage of the area is Marginally suitable, 24.21 percent of the area is marginally not suitable, 2.56 percent is permanently nor suitable and 1.71 percent of the area is moderately suitable for the cultivation of wheat in the Upper Cauvery area.
Adequate knowledge about the hydrology is very much required for the proper planning and management of water resources in an area. Rainfall and runoff are the important constituents in determining the hydrology of an area to determine the water management strategies. SCS- CN method is a widely used method for the calculation of surface runoff considering the land use pattern, soil type and antecedent moisture condition. In the present study runoff of the Palar watershed, Karnataka state, South India has been calculated using the SCS-CN method. The watershed consists of a total area of 2872.357 km2. The maximum rainfall of 1231.67 mm in the year 2005 and a minimum of 418.7 mm in the year 2003. The average annual runoff is calculated as 218.26 mm and 626.91MCM. The rainfall- runoff correlation value is 0.8253. The study results can be effectively coordinated for the watershed management activities.
An attempt has been made to develop water quality index (WQI), using Five water quality parameters pH, Nitrates, Chloride, electrical conductivity and fluoride measured at 137 different locations in the study area rating scale is developed based on FAO standards. It was found that 133 samples have the water quality index less than 150 and 4 samples have water quality index between 150-300. By spatial variation of WQI it can be found that 97.08 percent of the water in the area is excellently suitable for irrigation.
Intensity-duration-frequency (IDF) curves represent the relationship between storm intensity, storm duration and return period. The IDF curves available are mostly done by fitting series of annual maximum rainfall intensity to parametric distributions. Climate change is expected to exacerbate the extremes in the climate variables. Being prone to harsh climate impacts, it is very crucial to study extreme rainfall-induced flooding for short durations over regions that are rapidly growing. One way to study the extremes is by the application of the Intensity-Duration-Frequency (IDF) curves. The annual maximum rainfall intensity (AMRI) characteristics are often used to construct these IDF curves that are being used in several infrastructure designs for urban areas. Thus, there is a need to obtain high temporal and spatial resolution rainfall information. Many urban areas of developing countries lack long records of short-duration rainfall. The shortest duration obtained is normally at a daily scale/24 h. Thus, it is very crucial to find a methodology to construct IDF curves for short-duration rainfall (sub-daily) for these urban areas. The fast extension of urban area that does not have adequate preparedness to cope with climate change is certainly a big risk to life and economy. The study region is Upper Cauvery which lies in Karnataka India. The sub-daily IDF curves for current and future climate for Upper Cauvery were constructed from 1 to 24 h based on the Gumbel’s Distribution approach. Rainfall data of 23 (Twenty three) hydrological years of all stations were used. Maximum rainfall frequency analysis was made by Gumbel’s Distribution method. Finally Equations were developed for different return periods.
An attempt has been made to study the variability of seasonal and annual rainfall for a period of 25 years (19912015) for the upper Cauvery portion which has five districts. It can be observed that the average annual rainfall for every five years considered range from 800 to 1200mm for more than 45 percent of the area upto 2010 and from 2011-2015 it has been reduced to less than 35 percent and the percentage of area for which the rainfall range was less than 800mm was increased to 28.39 percent which was less than 14 percent from 1991-2010. The maximum portion of the area had average post monsoon rainfall between 100mm to 200mm has been from 1991 to 2010. And from 2011-2016 the maximum portion of the area has a average post monsoon rainfall less than 150mm. Some parts of Hassan, kodagu and chikkamangalore districts portions in the study area has average annual rainfall above 2000mm where as mandya district portion in the study area has annual rainfall less than 800mm and in mysore district average annual rainfall ranges from 800mm to 1500mm.
Accurate estimation of runoff and sediment yield amount is not only an important task in physiographic but also important for proper watershed management. Watershed is an ideal unit for planning and management of land and water resources. Direct runoff in a catchment depends on soil type, land cover and rainfall. Of the many methods available for estimating runoff from rainfall, the curve number method (SCS-CN) is the most popular. The curve number depends upon soil and land use characteristics. This study was conducted in the Upper Cauvery Karnataka using remote sensing and GIS. SCSCN method has been used for surface runoff estimation for Eight watersheds of Upper Cauvery. The soil map and land use were created in the GIS environment, because the curve number method is used here as a distributed model. The major advantage of employing GIS in rainfall -runoff modelling is that more accurate sizing and catchment characterization can be achieved. Furthermore, the analysis can be performed much faster, especially when there is a complex mix of land use classes and different soil types. The results showed that the surface runoff ranged from 170.12-599.84 mm in the study area, when rainfall rates were received from 1042.65-1912 mm. To find the relationship between rainfall and runoff rates, The straight line equation was used, That was found there a strong correlation between Runoff and precipitation rates, The value correlation coefficient between them was 86%. The Average depth of runoff is more in watershed A4, Average runoff coefficient is less in Watershed B2, the correlation coefficient is high in A4 to a value of almost 95%. Through of these results, the study recommends take advantage of runoff rates by reserving them at collection of Watershed and then using them for agricultural purposes in the vicinity. This would be better than reserving water from the total area which is 10874.65 square kilometers, and then will evaporate or infiltrate before reaching the dam lake
Engineering infrastructures such as storm water drains and bridges are commonly designed using the concept of Intensity-Duration-Frequency (IDF) curves, which assume that the occurrence of precipitation patterns and distributions are spatially similar within the drainage area and remain unchanged throughout the lifespan of the infrastructures (stationary). Based on the premise that climate change will alter the spatial and temporal variability of precipitation patterns, inaccuracy in the estimation of IDF curves may occur. As such, prior to developing IDF curves, it is crucial to analyse trends of annual precipitation maxima. The objective of this study was to estimate the precipitation intensities and their uncertainties (lower and upper limits) for durations of 5min, 10min, 15min, 30min, 60min,120min, 720min and 1440min and return periods of 2, 5, 10, 25, 50, 75 and 100 years in the Upper Cauvery Karnataka India using Pearson type III Values . The annual precipitation maxima were extracted from long-term (1995–2017) precipitation data for Forty Three meteorological stations sourced from the Water resources Development Organization Karnataka. On average, the estimated extreme precipitation intensities for the Study area ranged from 5.1 mm/h for 24 h storm duration to 226.01 mm/h for 5min at 100 years return period. At 50 year return period, the intensity ranged from 5.2 mm/h for 24h duration to 225 mm/h for the duration of 5min.
Intensity–duration–frequency (IDF) curves are among the most demandable information in meteorology, hydrology and engineering water resources design, planning, operation, and management works. The IDF Curves accessible are for the most part done by fitting arrangement of yearly greatest precipitation force to parametric dispersions. Intensity-durationfrequency (IDF) curves represent the relationship between storm intensity, storm duration and return period. Environmental change is relied upon to intensify the boundaries in the atmosphere factors. Being prone to harsh climate impacts, it is very crucial to study extreme rainfall-induced flooding for short durations over regions that are rapidly growing. One way to approach the extremes is by the application of the Intensity-Duration-Frequency (IDF) curves. The annual maximum rainfall intensity (AMRI) characteristics are often used to construct these IDF curves that are being used in several infrastructure designs for urban areas. Thus, there is a necessity to obtain high temporal and spatial resolution rainfall information. Many urban areas of developing countries lack long records of short-duration rainfall. The shortest duration obtained is normally at a daily scale/24 h. This paper suggests their generation based on annual daily maximum rainfall (ADMR) records. Rainfall data of 23 (Twenty three) hydrological years of all stations were used. Maximum rainfall frequency analysis was made by LogNormal Distribution method.
The IDF Curves accessible are for the most part done by fitting arrangement of yearly greatest precipitation force to parametric dispersions. Intensity-duration-frequency (IDF) curves represent the relationship between storm intensity, storm duration and return period. Environmental change is relied upon to intensify the boundaries in the atmosphere factors. Being prone to harsh climate impacts, it is very crucial to study extreme rainfall-induced flooding for short durations over regions that are rapidly growing. One way to approach the extremes is by the application of the Intensity-Duration-Frequency (IDF) curves. The annual maximum rainfall intensity (AMRI) characteristics are often used to construct these IDF curves that are being used in several infrastructure designs for urban areas. Thus, there is a necessity to obtain high temporal and spatial resolution rainfall information. Many urban areas of developing countries lack long records of short-duration rainfall. The shortest duration obtained is normally at a daily scale/24 h. Thus, it is very crucial to find a methodology to construct IDF curves for short-duration rainfall (sub-daily) for these urban areas. The fast extension of urban area that does not have adequate preparedness to cope with climate change is certainly a big risk to life and economy. The study region lies in Karnataka India. The sub-daily IDF curves for current and future climate for the region were constructed from 1 to 24 h based on the Normal Distribution approach. Rainfall data of 23 (Twenty three) hydrological years of all stations were used. Maximum rainfall frequency analysis was made by Normal Distribution method. Finally Equations were developed for different return periods.
Prioritization of watershed has Grabbed up significance in watershed management. Morphometic investigation is been usually applied to organize the watershed. In the present study upper cauvery of Karnataka with an area of 10874.65 km2 and highest order stream of 8 was considered. The area was divided into Eight Watersheds. Various morphometric parameters namely Bifurcation ratio(Rb), Drainage density (Dd), Stream frequency(Ns), Texture ratio(T), Form factor(Rf), Circularity ratio(Rc), Elongation Ratio(Re), length of overland flow, shape factor(Bs), compactness ratio (Cc) has been determined for each watershed and allotted position on premise of relationship as to arrive at a Compound value for final ranking of watershed. The morphometric parameters ranges between Rb (3.416-5.0442), Dd (1.377-1.463), Ns (1.397-1.579), T (5.2358.540), Rf (0.233-1.082), Rc (0.179-0.447), Re (0.545-1.173), Cc (1.496-2.365), Lof (0.341-0.363), and Bs (0.924-4.284). It is found that the 38.83 % of area falls under high priority category where as 42.12% of area falls under this Medium category and 19.05% of the area falls under low catergory.
Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. The Study Area lies between 750 29’ 19” E and 760 37’ 40” E longitude and 110 55’ 54” N and 130 23’ 12.8” N latitude. The study area covers an area of 10874.65 km2, having maximum length of 143.73 km. Drainage density is 1.43 km/km2 hence area is of coarse texture. The length of overlandflow is less than 0.4 indicating more runoff less infiltration. The study of hypsometric properties of watershed using hypsometric integral (HI) and hypsometric curve retrieved in that, HI value is 0.57 and hence watershed falls under the Mature Stage. Circularity ratio is 0.26 which shows that the drainage area is less circular.
Probable maximum precipitation (PMP) is widely used by hydrologists for appraisal of probable maximum flood (PMF) used for soil and water conservation structures, and design of dam spillways. The estimation of design storm for example depends on availability of rainfall quantities and their durations. Daily maximum multiannual series are one of the main inputs for design streamflow calculation. The study generated annual series of Daily maximum rainfall for fourty four stations by using statical approach such as Normal distribution, Log-Normal Distribution, Pearson type III distribution and Gumbel’s Distribution .Results reveals that among the different statical approaches Log-Normal distribution fits the best compared to others. Isohyetal Maps of study area at different frequency are produced by using GIS tools, the maximum intensity varies from 2.5 mm/hr to 628 mm/hr.
Runoff is one of the most significant hydrological variables used in most of the water resources applications. Physiographically the area is characterized by undulating topography with plains and valleys. The Soil Conservation Service Curve Numbers also known as hydrologic soil group method were used in this study. This method is adaptable and suitable approach for quick runoff estimation and is approximately easy to use with minimum data and it gives good result. From the study yearly rainfall and runoff were estimated easily. The study area covers an area of 466.02 km2, having maximum length of 36.5 km. The maximum and minimum elevation of the basin is 569 m and 341 m above MSL, respectively.
Changes in the hydrologic cycle due to increase in greenhouse gases cause variations in intensity, duration, and frequency of precipitation events. Quantifying the potential effects of climate change and adapting to them is one way to reduce urban vulnerability. Since rainfall characteristics are often used to design water structures, reviewing and updating rainfall characteristics (i.e., Intensity–Duration–Frequency (IDF) curves) for future climate scenarios is necessary. The present study regards the evaluation of the IDF curves for Four raingauge stations of Bangalore rural : Anugondanahalli, Devanahally, Doddabalapura and Hoskote. Starting from daily rainfall observed data, to define the IDF curves and the extreme values in a smaller time window (2, 5, 10, 15, 30, 60, 120, 720, 1440 minutes), disaggregation techniques of the collected data have been used, in order to generate a synthetic sequence of rainfall, with statistical properties similar to the recorded data. Then, the rainfall pattern of the Four raingauge stations was analyzed and IDF curves were evaluated
Unit Hydrograph (UH) is the most famous and generally utilized technique for analysing and deriving flood hydrograph resulting from a known storm in a basin area. For ungauged catchments, unit hydrograph are derived using either regional unit hydrograph approach. Central Water Commission (CWC) derived the regional unit hydrograph relationships for different sub-zones of India relating to the various unit hydrograph parameters with some prominent physiographic characteristics. In this study, the lately developed UH model is applied located between Latitude 15º54′2′′ N to 16º16′19′′ N Latitude and 76º48′40′′ E to77º4′21′′ E Longitude. The study area covers an area of 466.02 km2, having maximum length of 36.5 km. The maximum and minimum elevation of the basin is 569 m and 341 m above MSL, respectively. The Peak discharge of unit hydrograph obtained is 171.58m3/s. The final cumulative discharge is 1669.05 m3/s.
Unit Hydrograph (UH) is the most famous and generally utilized technique for analysing and deriving flood hydrograph resulting from a known storm in a basin area. For ungauged catchments, unit hydrograph are derived using either regional unit hydrograph approach. Central Water Commission (CWC) derived the regional unit hydrograph relationships for different sub-zones of India relating to the various unit hydrograph parameters with some prominent physiographic characteristics. The Study Area is located between Latitude 15º57′58′′ N to 16º11′25.6′′ N and 77º18′1′′ E to77º32′5.3′′ E Longitude and covers area of 360.97 km2, having maximum length of 26.17 km. The maximum and minimum elevation of the basin is 533 m and 323 m above MSL, respectively. The Peak discharge of unit hydrograph obtained is 311.469 m3/s. The final cumulative discharge is 1458.55 m3/s.
In this study the calculation procedure and comparative results of IDF curves for the area of Mandya are presented. Rainfall data of 19 (Ninteen) hydrological years of stations Srirangapatna, Kikkere and Bindganarole were used. Maximum rainfall frequency analysis was made by Four methods (Normal, Gumbel, Pearson type III and logarithmic Pearson type III) and subsequently the IDF curves with Four methods (two forms of excessive functions and a polynomial function) were exported. Finally, comparative testing with the IDF which were prepared by Chisquare test and it was found that the log-normal distribution suits the best fit for all the stations considered.
Aam Talaab also known as Maavina Kere or mango beach is one of the major attractions of Raichur. It is located between Latitude 16º10′49.5′′ N to 16º11′27.8′′ N Latitude and 77º20′36′′ E to 77º23′26′′ E Longitude and an area of 4.77 km2, having maximum length of 3.98 km. The maximum and minimum elevation of the basin is 491 m and 404 m above MSL, respectively.
The water balanced of a place, whether it be an agricultural field, watershed, or continent, can be determined by calculating the input, output, and storage changes of water at the Earth's surface. The major input of water is from precipitation and output is evapotranspiration. The water balance is intended for use as a screening tool to further evaluates water resources allocations within the watershed and to identify water balance components that may require further analysis during the next levels of watersheds planning. The study area chosen for the present study area is Doddavalabhi sub watershed which falls in Kolar taluk of Kolar district. The study areas geographically lies between 760 8’ 0” E and 760 23’ 0” E longitude and 120 20’ 0” N and 120 28’ 0” N latitudes with an area 15.20 sq.km. For the determination of crop water requirement for Kolar major crops considered are ragi and groundnut with the crop period of 120 days and 140 days respectively. The year and monthly wise potential evapotranspiration and actual evapotranspiration is calculated by using penman method, blaney-criddle method, pan evaporation and radiation methods. The year wise potential evapotranspiration calculated by Blaney-criddle is maximum 645.66 mm during 2014, in this year monthly PET is maximum in July month ie 150.4mm. The year wise potential evapotranspiration calculated by Pan Evaporation is maximum 236.43 mm during 2014, in this year monthly PET is maximum in July month ie 56.67mm. The Year wise actual evapotranspiration is also maximum during 2014 for both ragi and groundnut. Hence Blaney criddle method is best suitable since it provides the most satisfactory results compared to other methods because this method is suggested for areas where available climatic data cover air temperature data only.
In developing accurate hydro geomorphological analysis, monitoring, ability to generate information in spatial and temporal domain and delineation of land features are crucial for successful analysis and prediction of groundwater resources. However, the use of RS and GIS in handling large amount of spatial data provides to gain accurate information for delineating the geological and geomorphological characteristics and allied significance, which are considered as a controlling factor for the occurrence and movement of groundwater used IRS LISS II data on 1: 50000 scale along with topographic maps in various parts of India to develop integrated groundwater potential zone
Student information management system project report ii.pdfKamal Acharya
Our project explains about the student management. This project mainly explains the various actions related to student details. This project shows some ease in adding, editing and deleting the student details. It also provides a less time consuming process for viewing, adding, editing and deleting the marks of the students.
About
Indigenized remote control interface card suitable for MAFI system CCR equipment. Compatible for IDM8000 CCR. Backplane mounted serial and TCP/Ethernet communication module for CCR remote access. IDM 8000 CCR remote control on serial and TCP protocol.
• Remote control: Parallel or serial interface.
• Compatible with MAFI CCR system.
• Compatible with IDM8000 CCR.
• Compatible with Backplane mount serial communication.
• Compatible with commercial and Defence aviation CCR system.
• Remote control system for accessing CCR and allied system over serial or TCP.
• Indigenized local Support/presence in India.
• Easy in configuration using DIP switches.
Technical Specifications
Indigenized remote control interface card suitable for MAFI system CCR equipment. Compatible for IDM8000 CCR. Backplane mounted serial and TCP/Ethernet communication module for CCR remote access. IDM 8000 CCR remote control on serial and TCP protocol.
Key Features
Indigenized remote control interface card suitable for MAFI system CCR equipment. Compatible for IDM8000 CCR. Backplane mounted serial and TCP/Ethernet communication module for CCR remote access. IDM 8000 CCR remote control on serial and TCP protocol.
• Remote control: Parallel or serial interface
• Compatible with MAFI CCR system
• Copatiable with IDM8000 CCR
• Compatible with Backplane mount serial communication.
• Compatible with commercial and Defence aviation CCR system.
• Remote control system for accessing CCR and allied system over serial or TCP.
• Indigenized local Support/presence in India.
Application
• Remote control: Parallel or serial interface.
• Compatible with MAFI CCR system.
• Compatible with IDM8000 CCR.
• Compatible with Backplane mount serial communication.
• Compatible with commercial and Defence aviation CCR system.
• Remote control system for accessing CCR and allied system over serial or TCP.
• Indigenized local Support/presence in India.
• Easy in configuration using DIP switches.
Sachpazis:Terzaghi Bearing Capacity Estimation in simple terms with Calculati...Dr.Costas Sachpazis
Terzaghi's soil bearing capacity theory, developed by Karl Terzaghi, is a fundamental principle in geotechnical engineering used to determine the bearing capacity of shallow foundations. This theory provides a method to calculate the ultimate bearing capacity of soil, which is the maximum load per unit area that the soil can support without undergoing shear failure. The Calculation HTML Code included.
CFD Simulation of By-pass Flow in a HRSG module by R&R Consult.pptxR&R Consult
CFD analysis is incredibly effective at solving mysteries and improving the performance of complex systems!
Here's a great example: At a large natural gas-fired power plant, where they use waste heat to generate steam and energy, they were puzzled that their boiler wasn't producing as much steam as expected.
R&R and Tetra Engineering Group Inc. were asked to solve the issue with reduced steam production.
An inspection had shown that a significant amount of hot flue gas was bypassing the boiler tubes, where the heat was supposed to be transferred.
R&R Consult conducted a CFD analysis, which revealed that 6.3% of the flue gas was bypassing the boiler tubes without transferring heat. The analysis also showed that the flue gas was instead being directed along the sides of the boiler and between the modules that were supposed to capture the heat. This was the cause of the reduced performance.
Based on our results, Tetra Engineering installed covering plates to reduce the bypass flow. This improved the boiler's performance and increased electricity production.
It is always satisfying when we can help solve complex challenges like this. Do your systems also need a check-up or optimization? Give us a call!
Work done in cooperation with James Malloy and David Moelling from Tetra Engineering.
More examples of our work https://www.r-r-consult.dk/en/cases-en/
Industrial Training at Shahjalal Fertilizer Company Limited (SFCL)MdTanvirMahtab2
This presentation is about the working procedure of Shahjalal Fertilizer Company Limited (SFCL). A Govt. owned Company of Bangladesh Chemical Industries Corporation under Ministry of Industries.
Forklift Classes Overview by Intella PartsIntella Parts
Discover the different forklift classes and their specific applications. Learn how to choose the right forklift for your needs to ensure safety, efficiency, and compliance in your operations.
For more technical information, visit our website https://intellaparts.com
Vaccine management system project report documentation..pdfKamal Acharya
The Division of Vaccine and Immunization is facing increasing difficulty monitoring vaccines and other commodities distribution once they have been distributed from the national stores. With the introduction of new vaccines, more challenges have been anticipated with this additions posing serious threat to the already over strained vaccine supply chain system in Kenya.
COLLEGE BUS MANAGEMENT SYSTEM PROJECT REPORT.pdfKamal Acharya
The College Bus Management system is completely developed by Visual Basic .NET Version. The application is connect with most secured database language MS SQL Server. The application is develop by using best combination of front-end and back-end languages. The application is totally design like flat user interface. This flat user interface is more attractive user interface in 2017. The application is gives more important to the system functionality. The application is to manage the student’s details, driver’s details, bus details, bus route details, bus fees details and more. The application has only one unit for admin. The admin can manage the entire application. The admin can login into the application by using username and password of the admin. The application is develop for big and small colleges. It is more user friendly for non-computer person. Even they can easily learn how to manage the application within hours. The application is more secure by the admin. The system will give an effective output for the VB.Net and SQL Server given as input to the system. The compiled java program given as input to the system, after scanning the program will generate different reports. The application generates the report for users. The admin can view and download the report of the data. The application deliver the excel format reports. Because, excel formatted reports is very easy to understand the income and expense of the college bus. This application is mainly develop for windows operating system users. In 2017, 73% of people enterprises are using windows operating system. So the application will easily install for all the windows operating system users. The application-developed size is very low. The application consumes very low space in disk. Therefore, the user can allocate very minimum local disk space for this application.
Final project report on grocery store management system..pdfKamal Acharya
In today’s fast-changing business environment, it’s extremely important to be able to respond to client needs in the most effective and timely manner. If your customers wish to see your business online and have instant access to your products or services.
Online Grocery Store is an e-commerce website, which retails various grocery products. This project allows viewing various products available enables registered users to purchase desired products instantly using Paytm, UPI payment processor (Instant Pay) and also can place order by using Cash on Delivery (Pay Later) option. This project provides an easy access to Administrators and Managers to view orders placed using Pay Later and Instant Pay options.
In order to develop an e-commerce website, a number of Technologies must be studied and understood. These include multi-tiered architecture, server and client-side scripting techniques, implementation technologies, programming language (such as PHP, HTML, CSS, JavaScript) and MySQL relational databases. This is a project with the objective to develop a basic website where a consumer is provided with a shopping cart website and also to know about the technologies used to develop such a website.
This document will discuss each of the underlying technologies to create and implement an e- commerce website.
Quality defects in TMT Bars, Possible causes and Potential Solutions.PrashantGoswami42
Maintaining high-quality standards in the production of TMT bars is crucial for ensuring structural integrity in construction. Addressing common defects through careful monitoring, standardized processes, and advanced technology can significantly improve the quality of TMT bars. Continuous training and adherence to quality control measures will also play a pivotal role in minimizing these defects.