عنوان

بررسی انطباق طرح های توسعه جدید شهری با معیارهای نوشهرگرایی( مطالعه موردی : منطقه نه شهرداری تبریز)

شماره

‭۱۳۸۴۳پ‬

زبان متن نوشتاري يا گفتاري و مانند آن

per

عنوان اصلي

بررسی انطباق طرح های توسعه جدید شهری با معیارهای نوشهرگرایی( مطالعه موردی : منطقه نه شهرداری تبریز)

نام نخستين پديدآور

/میر ابوالفضل صدرموسوی گرگری

نام ناشر، پخش کننده و غيره

: پردیس دانشگاه تبریز

تاریخ نشرو بخش و غیره

، ‮‭۹۴‬

متن يادداشت

چاپی

جزئيات پايان نامه و نوع درجه آن

کارشناسی ارشد

نظم درجات

جغرافیا و برنامه ریزی شهری

زمان اعطا مدرک

‮‭۱۳۹۴/۰۶/۲۹‬

کسي که مدرک را اعطا کرده

تبریز

متن يادداشت

اگرچه قدمت دانش نوشهرگرایی سابقه ای دیرینه دارد، ولی معانی و مفاهیم روشنی از آن در دانش نوشهر گرایی تخصصی در زمان معاصر ارائه نگردیده است .براساس تعریفی که از نوشهرگرایی ارائه میشود می توان گفت که نوشهر گرایی در جهت رفع مشکلات ناشی از فرسودگی و زوال مراکز شهری و گسترش افقی شهرها به وجود آمده است .هدف اصلی از انجام این تحقیق، بررسی انطباق طرحهای توسعه جدید شهری منطقه نه شهرداری تبریز با معیارهایی که برای نوشهرگرایی ارائه میشود، می باشد .روش کاری که برای انجام این تحقیق به کار گرفته شده ، بهره گیری از منابع کتابخانه ای و تحقیقات محلی و میدانی، گرفتن اطلاعات و منابع داده ای از مراکز و سازمانها و مسئولین مربوطه بوده و پس از جمع آوری داده ها وبه دلیل نبود و عدم ارایه اطلاعات از سوی مراجع ذیصلاح تا حدودی توانستیم میزان انطباق منطقه نه شهرداری تبریز با اصول نوشهر گرایی بیان کنیم که طی این مطالعه معلوم گردید که میزان انطباق اصول پیاده مداری ،حفظ و تقویت فضاها و اتصال و پیوستگی دارای بیشترین درجه و اصل حمل و نقل هوشمند دارای کمترین درجه در منطقه مورد مطالعه بوده است .

متن يادداشت

Soil is a functional of the pedogenic factors that has reached development by affecting of influence processes. Studying soil development is one of the identification methods to survey soil historical changing and evolution. Micromorphologic studying can be one of the appropriate ways for examining formation and the evolution of soils. Micromorphologists have used software- image analyzing to quantification of some soil fabric properties that cause increasing speed, precision and micromorpholgical studying ability. Also, using some factors and indexes to quantification of horizontals improvement have been reported, for example can mention to Micromorpholgical Index of soil Evolotion Calcareous arid to semiarid Condition (MISODI) and micromorpholgical index Evolotion of non-calcic soils (MISECA). MISODI index is used as index of Evolotion degree of non-calcic soils association with microstructure, B-fabric, clay coating, nodols and mineral weathering degree factors, whereas MISECA is used as calcic soil improvement Index of soil Evolotion Calcareous arid to semiarid Condition association with micro structure, B-fabric, clay coating, calcic depletion area, iron oxidation to manganese rate and mineral weathering factors. In this studying at Kaleibar Chaieh Sofla on four different position slope including; Shoulders, Backslopes, Footslopes and Toeslopes were drilled and from each horizon altered and undisturbed Sample were prepared by Kobiana box. Samples transferred to laboratory in order to do physical, chemical and micromorpholgical analyses. After preparation of Thin sections total number, Roundness, perimeter, circularity, fractal dimension, and soil pore area was calculated by ImageJ2 version Fiji. Acquired data was surveyed through complete randomly design. In addition, picture prepared from each soil profile and including parameters such as nodols, microstructure, B-fabric, clay coating, calcic depletion area, Fe/Mn oxidation and mineral weathering degree in each index identified based on those grading and finally Evolotion degrees and soils evolution was identified. Results were compared with MISECA and MISODI models. Comparison revealed, in spite of MISECA models had offered to very calcic soil in drought area, us calculation at different positions shown more moisture in forest soils with dioxide carbon caused by biological activity lead to calcium carbonate be solve and accumulate at lower deeps. Also, MISODI become preference because of more detailed divides (for example micro divided microstructure). In addition, the types of pore present at the surface of horizons mostly were channel and merged type and a little.Vughs But, in lower layers was observed that pore type became changing and mostly Vughs, channel, plate, and a little merged. Area, perimeter, fractal dimension, total number, Roundness,equivalent pore diamater(EPD) and circularity pores among four slope position were significant. Maximum and minimum amount were at surface deep and lower deep, respectively. The circulation circularity degree of soil pore shape was extensive. In lower deep relative percentage with extensive circulation was less and soil pore total number was high. Among soil physical and chemical properties, that had high relationship with soil pore properties, can mention to organic material, sand, clay, and calcic. As results, these properties can have a direct or indirect effect on pore size distribution. Totally, this studying reveals micromorpholgical techniques and Image analysis with together can trace different slope and deeps effect on the properties of soil pores size at various position. In addition, MISECA model was better than MISOD model for the categorization surveying of studying area

مستند نام اشخاص تاييد نشده

صدرموسوی گرگری، میرابوالفضل

مستند نام اشخاص تاييد نشده

روستایی، شهریور، استاد راهنما

مستند نام اشخاص تاييد نشده

اصغری زمانی، اکبر، استاد مشاور

يادداشت عمومي

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