فهرست مطالب mohsen barzkar

The concept of morphometry involves the measurement and numerical analysis of land surface, shape, dimensions and form of land. In relation to flooding, watershed morphometry includes quantitative indicators describing watershed physical characteristics that control the pattern and quantitative characteristics of floods such as amount, time of occurrence, delay time, and flow hydrograph. Unusual development of cities due to population growth and consequent land use change has caused disruption of hydrological balance and increased flooding of basins. The purpose of this study was to prioritize the sub-catchments of Zab River based on a novel combination of morphometric analysis and statistical correlation and zoning of flood potential under sub-catchments.

to disregard for human and social sub-basins, which has a great impact on the hydrological processes of the catchment. Based on the validation results, the Shinabad and Sufian basins have the highest priority, and the new method of morphometric analysis and statistical correlation have considered them the highest priority for managers' attention.The elongation ratio helps to understand the hydrological characteristics of the drainage basin and ranges from 1 for circular basins to 0 for extended basins and its high values ​​indicate the shape of the basin circle, high peak discharge and high flood potential. Is. The values ​​of tensile strength in all sub basins are more than 0.5 and indicate high potential for flooding. Straller (1964) considers the circle ratio a quantitative measure for visualizing the shape of the basin. High values ​​of this parameter indicate circular shape, high to medium ruggedness and low permeability in the basin, which causes peak discharge in less time. The ratio of the circular ratios under the Lavin Tea Basins is 0.17, Copar 0.19, and Zab Small 0.27, indicating relatively low flooding potential in this parameter. The amount of this parameter is 0.35 under Shinabad basin and 0.31 under Sufian basin which indicates their higher flood potential in this parameter (Table 7). The branching ratio is an important parameter affecting peak runoff hydrograph discharge with high values ​​indicating high instantaneous discharge and flood event. The mountainous and steep areas have a split ratio of 3 to 4. Branching ratio values ​​indicate low flooding potential except for Shinabad basin which shows this ratio of 6.19 and this ratio indicates high flood potential
 

Since hydrological units are based on morphometric parameters to prioritize flood mapping, firstly, using channel networks and elevation curves, topographic maps of 1: 50000 and digital elevation data are analyzed. The boundaries of the hydrological units became. Then, because the catchment morphological parameters have different effects on soil erosion processes and runoff formation, prioritization of the sub-basins was done in a new way based on the difference of morphological parameters and statistical correlation analysis between them. Morphometric parameters were calculated for all sub-basins in GIS software. Then, statistical correlation of morphometric parameters was performed based on the t-Kendall method using SPSS software. Based on the correlation matrix we can analyze the relationship between the parameters and define the relative weight for each parameter without All twelve variables including circular elongation ratio, branching ratio, flow frequency, drainage density, drainage texture, compaction index, shape factor, mean slope, roughness ratio, roughness, and roughness number for all sub-basins are calculated in Table 2. The Kendall correlation coefficient was used to investigate the relationship between Validation results showed that the new method of morphometric analysis and statistical correlation did not perform well in prioritizing all sub-basins, but this method was accurate in identifying the most priority sub-basins (most acute conditions). The reason for this may be due to the lower performance of morphometric analysis and the characterization of waterways in low-slope catchments. Also, the precise reason for not estimating the priority of some sub-basins is due.

The selected twelve parameters are directly related to runoff and flood potential. Therefore, high values ​​of parameters have a direct relationship with runoff and flood potential due to their greater impact on the selected twelve parameters. Indicator (Cv) values ​​for each sub-basin are obtained from averaging of 12 indices and accordingly sub-basins of Shinabad and Sufis with high flood potential, sub-basin with small potential and sub-basin zab basin. Copar and Lavin Tea have physiographic and morphometric characteristics of the sub-catchments have a great influence on flooding and hydrological behavior, it is possible to study the status and potential of flooding below the catchments. In this research, in order to potential of flooding, firstly, Zab sub-basins were prioritized based on the new method of morphometric analysis and statistical correlation. Based on this method, the results showed that the Shin abad and Sufi basins are the top priority for the implementation of management measures to ensure.

Rivers are one of the best geomorphic landscapes in which the connection between the system of forces and the forms of unevenness can be clearly understood (Chorley et al., 2000: 163). Various sites, especially sedimentology, are important. Zab River is one of the most water-rich rivers in the country, which due to the high discharge, causes a lot of damage annually due to floods on agricultural lands located in the river. This river, by changing its course in the bed and creating erosion along the bed, exposes the lands around the bed to destruction, and considering that the farmers of the region use the river water for agriculture, it is of great economic importance for them.Therefore, it is necessary to classify and determine the boundaries of the riverbed and thus understand the existing processes and morphological knowledge of it. Therefore, it is necessary to classify and determine the boundaries of the riverbed and, as a result, to understand the existing processes and its morphological knowledge.

River classification according to Rosegan method Rosegan classification is divided into four levels: In this research, for the morphological classification of Zab river, first by scrolling along the study area, an almost uniform set of geomorphic units is identified. Then, using GPS in three paths upstream, middle and downstream of the study area were segmented. After intercepting the river route and then entering the required data into the WMS9.1 and HEC-RAS software environment and executing the hydrological model, the geometric properties of 24 transverse sections of the total sections in all intervals The studied route was extracted and all the parameters required for classification and geometry of the duct in those intervals were calculated. To determine the overflow discharge of the intervals, the discharge with different return periods obtained from the relationship between Fuller and smada software with The prepared sections were given to HEC-RAS software and then based on one of the methods to determine the full cross section (level at which the ratio of width to depth to depth in an orthogonal device is minimized) the overflow flow is determined Took. Accordingly, in each cross section of the curve, the ratio of width to depth of flow versus depth for each section was plotted and the minimum point on the curve was selected as the discharge of the full section. After determining this discharge in each transverse section, using frequency analysis, the full section discharge has been determined for the whole river. Finally, by introducing flow characteristics, geometric characteristics and manning coefficient of each section in HEC-RAS software, flow simulation was performed and data related to cross-sections and water surface profiles including width to depth ratio, indentation index Bed, cross-sectional area in overflow, overflow width, maximum depth, flood plain width and water level slope, etc. were calculated. The implementation steps of the HEC-RAS model are shown in Figure 2.

According to field and laboratory studies, Zab River is in the alluvial group in terms of classification based on the type of bed sediments (rocky and alluvial). In summer, due to dehydration, fine-grained sediments are placed on coarse-grained sediments, as a result of which sand particles get stuck between the sand particles and cause the bed to solidify. These sediments are sandy but in winter Due to the flood, fine particles are displaced along with the flood and large particles remain at the bottom of the bed, so the type of sediments on the bottom of the Zab River are sandy. To obtain the average size of duct material, 15 samples were taken along the river at different distances and granulated in the laboratory. Due to the fact that the intervals 4 in the upstream and 11 in the middle part of the studied route have a mixed bed of irregular rapids or erosion basins and the bed (profile) and sides are relatively stable and have a limited sediment transport system with type B Roses are compatible. Also, moderate roughness and narrow valleys with a gradual slope are other reasons for confirming this claim. Intervals 1, 2, 3, 4, 5 upstream, 10, 12, 13, 14 in the middle and 17, 20, 21, 22, 23, and 24 downstream of the studied route with respect to stability They and their sediment load and limited transport are Type C compliant. The predominant morphological feature of these areas is wide valleys with alluvial terraces associated with the flood plain, which are again the characteristics of this type. Section 18 is located in the downstream part of the studied route in type D, which is witnessed by the following reasons. The river is arterial in this area and rock fragments are rarely seen in the bed. The ducts also have erodible edges and high suction load. The morphological appearance of most areas has this type of wide valleys with alluvial and clovial cones. Interval 12 is located in the middle part of the studied route in type E. Here the ducts show significant sinusitis and the ratio of width to depth is low. The river is stable in this area and one of the reasons is the development in the floodplain with dense grass cover on the vertical shore of the duct. The predominant morphological feature of this section is the type of wide valleys with grasslands.

The characteristics of these intervals indicate their conformity with the Rosgen model. High instability of the riverbed in the range of intervals of types C and D is a threat to agricultural lands and surrounding structures. The results of evaluating the stability conditions of the intervals of the study area in the third level of Rozgan showed that in the upstream path of the study area, the intervals of 2, 5, and 8 intervals have more stable conditions at a good level than other intervals. Flow conditions in the intervals 1, 3, 6, 7 are at the intermediate level and in the interval 4 are at the weak level, which have more unstable conditions. In the intermediate path, the range 11 is better and more stable, and the 10, 12, 13, and 15 ranges are at the intermediate level, which is less stable. In the downstream direction, the studied areas are intervals 19, 21 and 22 at a good level and with more stable conditions, intervals 18, 20, 23 and 24 at a medium level and range 17 at a weak level and instability conditions. The results of Zab River evaluation based on Rozgan classification system at levels two and three showed that the canal patterns in Zab River and consequently the effective parameters in classifying and separating the canals are consistent with Rozgan system. However, there are differences in the values ​​and parameters that are due to specific conditions of local influencing factors. However, the Rozgan system is responsible for the morphological knowledge of the Zab River and similar fluvial systems. کرد. Therefore, this model has the ability to quantitatively predict the geomorphism of the Zab River and rivers with similar conditions.

The habitat development and establishment are directly related to the natural bedrock and geomorphologic complications. Due to topographical and geological conditions, the area under study has certain limitations in locating and developing human settlements. In order to reduce the hazards in the southeast of Khorasan Razavi province and modify plans for the development and establishment of human settlements, the feasibility of the area under study for residential development was investigated. After conducting library and field studies and selecting appropriate criteria, the fuzzy logic model was applied using the GIS software to identify areas for habitat development and establishment. In this study, to identify the potential areas for habitat development and establishment based on geomorphologic landforms, eleven parameters – including slope, slope direction, elevation, soil, land use, elevation, distance from fault, distance from river, distance from road, distance from settlement, and geomorphology – were used as independent variables in identifying geomorphological abilities and bottlenecks in the area. The results of zoning based on the fuzzy model showed that about 61% of the study area is located in very inappropriate and inappropriate classes, which means that geomorphological conditions in this part of the study area are unfavorable for the development and establishment of human settlements. About 14.58% of the study area has moderate conditions and about 24% of the study area shows favorable geomorphological conditions for construction activities and creation of new habitat areas. Alluvial fan units and alluvial plains are the most suitable sites for habitat development and establishment.

Introduction Ecological capability assessment (landuse planning) as follows: Regulate the relationship between man, land and human activities on land to sustainable use of all human resources and land space to improve the material and spiritual position in the course of time. Planning recreational outing as a way of protection functions in the areas of natural resources management work experience, they also provide the dynamic field of protection (Laurance at all, 2005: 457). Recreationplanning as a strategy management experience in the areas of natural resources, provide dynamic conservation (Laurance at all, 2005: 457). The aim of this study is Zoning Planning with the approach of ANP and AHP models for tourism development. Based on multi-agent approach to special assessment process network analysis is based on various environmental data. These models are presented based on various environmental data. This research ultimately assessment and will identify has the ability to develop tourism zones in the city limits of Oshnavieh. The results of this research can be used as an indicator for the development of appropriate and optimum applications.
Materials & Methods Oshnavieh city located in the southwestern province of West Azerbaijan. In this study, in order to landuse planning for tourism development with evaluation of a multi- factor approach, were used for the study area of 10 variables Elevational classes, slope, aspect, soil, lithology, land cover, road of communication, fault, flood potential and landslide potential. In this study, different maps with different scales, RC GIS10 and Super Decisions software are used. In the nextstage were valuation variables using the ANP and AHP models based on expert opinion. Then, was prepared the desired output of the reference maps by using of analysts spatial in GIS and the overlaying this maps in GIS environment by using Algebraic sum, respectively the final output as land use zoning scheme for the development of spatial tourism. Distributed were 15 questionnaires among specialists for each model (5 specialist land use, 5 tourism specialist and 5 specialist geomorphology) for valuation. After analyzing the questionnaires, to calculate the final weights of each criteria and sub-criteria (according to internal communications) was used Super Decisions software.
Results & Discussion In this study, were determined the evaluation criteria and their weights, correctly and with acceptable accuracy (under 1/0) by reviewing the literature, experts and paired in the form of ANP and AHP. Finally after the overlay was obtained zoning map for tourism development model based on AHP and ANP in the city Oshnavieh. The maps are in three categories: permitted, conditional and prohibited zones classified and the area was calculated. In the ANP model 7/21 percent and inthe AHP 1/21 percent of the study region has a permitted of tourism development and capability are better for tourism development. Most of the area has a slope between 0 to 8 percent and also the type of pasture lands are semi-intensive. The potential forflooding and landslides in these areas is low and very low so these areas are ecologically appropriate land use is extensive. Because the user of nature tourism is compatible with all users within this class. Conditioned class included 8/42 percent in model ANP and 42/08 percent in AHP model in the study area. In these areas, provided that the adherence to ecological aspects of development are extensive. Prohibited class included about 36 percent of the region. Any tourism development is prohibited becauseof its agricultural land and steep in parts, potential flooding and landslides. A large part of central and northern parts of the East region's capacity for sustainable development of tourism show better. Although these results are based on two models aredifferent, but generally close together.
Conclusion The results were calculated in three quality groups: Permited, forbidden and conditional. It was revealed that 21 percent of the area had the capacity for permited degree of tourism development and about 42 percent of the area had the conditional degree of tourism development conciderring ecologic prespectives. In the remaining 37 percent of the area tourism development was forbidden under any condition. In areas that have been allowed to develop tourism if desired, providedthe facilities and utilities and their potential to develop sustainable tourism could be promoted properly and economic equilibrium and balance different areas, especially in underdeveloped and rural use. The results of this study can be was exploited asan indicator for the development of appropriate landuses and optimize in the framework economic projects in the region.

Geomorphotourism is a branch of geosciences and tourism studies, which studies the geomorphosites or geomorphological special locations.In this research geotourism potentials of geomorphosites in Mahabad county were analyzed based on new techniques such as Comanescu method and field studies.Values resulted from each method were compared with each other, and the scientific, cultural, economic, management, and beauty values of the sites were analyzed by Comanescu method.Geotouristic valuation of each Geomorphosite is of paramount importance in tourism planning and investment respecting the geomorphotouristic potentials of the area.Among the examined landforms, Saholan water cave was found to have the highest score of 75.