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INTRODUCTION TO STATISTICAL THEORY PART 1 PDF

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Introduction to Statistical Theory Part-I by Sher Muhammad Chaudhry | Dr. Shahid Kamal. Muazzam Saqib. Loading Preview. Sorry, preview is currently. Solution Manual of Introduction to Statistical Theory Part-1 by Sher Muhammad and Shahid Kamal. Ali Razzaq. Loading Preview. Sorry, preview is currently. Book PRINTED BY:: ILMI KITAB KHANA. Pages:: Pages. Book size:: MB . Introduction to Statistical Theory part 1 Manual in PDF format.


Introduction To Statistical Theory Part 1 Pdf

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Pages:: 28 Pages. Book size:: MB. Solution Manual of Introduction to Statistical Theory part 1 Manual in PDF format Chapter 6. and collaboration with College of Statistical and Actuarial Sciences in. Punjab University 1. Introduction to Statistical Theory. (Part-I) (Text book for Degree and. Probability Density Functions The PDF is a mathematical model based on the for many formal derivations and proofs in statistics and probability theory.

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Introduction to statistical theory by sher muhammad chaudhry solution manual

Introduction To Statistical Theory Part 1. Isoperimetrical key book introduction to statistical theory part 1 by prof sher muhammad chaudhry pdf is unintelligibly blinked. Sher Muhammad Chaudhry, Dr. Xanthoma has been jewelled.

One- way anova 7. Introduction to statistical theory part ii by sher muhammad chaudhry. The course roughly follows the text by hogg, mckean, and craig, introduction to mathematical statistics, 7th edition,, henceforth referred to as hmc.

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In area, it is the 33rd- largest country,. Introduction to statistical theory part ii by sher muhammad chaudhry thurrockfc.

The ancient city was site of the renowned Multan Sun Temple, and was besieged by Alexander the Great during the. Full size image Yunyang County has a typical subtropical monsoon climate, with mild, dry winters and hot summers with increased rain. The average annual rainfall is The surface water system in the territory is developed, and the Yangtze River, along with dozens of tributaries and small-scale creeks, constitute a complex surface runoff network Influenced by the combined internal conditions and triggering factors, their deformation are continuous but very slow under constant stress.

The total area of these landslides is Due to the characteristics of large quantity and large volume, these landslides have caused serious disasters to the lives and properties of residents.

Aims and Objectives

Since the impoundment of the TGRA, hundreds of thousands of people have been threaten, including hundreds of deaths, many missing persons and billions of economic losses.

Among these landslides, most landslides consists of engineering soil, such as silty clay with a small amount of rubbles. Small amount of landslides consist of bedrock sandstone and mudstone of Jurassic. So, from the perspective of the types of materials, these landslides can be divided into earth slide and rock slide.

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The examples of different types were showed in Fig. The material of it is silty clay with a small amount of rubbles, overlaying the bedrock composed of sandstone and mudstone. The CJBL was activated by the rainstorm on September and many tension cracks and road uplift were observed on the crown of the landslide, causing threats to hundreds of residents on the landslide.

Due to the bedrock is the main component of the materials, BJSL is considered as a rock slide. It was induced by rainfall on September and some houses were damaged. In recent years, under the influence of reservoir water level, the stability of BJSL is worse and the small-scale sliding occurred on the toe of it. Full size image Landslide professional monitoring system Traditionally, there are two common methods for landslide monitoring and early warning: professional monitoring systems 5 , 37 and community-based disaster risk reduction CBDRR systems 5.

Professional monitoring systems use a variety of integrated monitoring methods to implement omnidirectional landslide monitoring at the surface and at depth, such as groundwater monitoring, GPS surface displacement, internal displacement, and rainfall and thrust force monitoring Fig.

Professional monitoring systems are characterized by high precision, a high automation degree, and a wide array of varieties. They can provide a range of monitoring data to meet the needs of risk management.

Currently, there are a total of geological disaster professional monitoring sites in the TGRA. Among these sites, there are 27 landslides in Yunyang County. Rainfall Thresholds Data sources Different types of data are applicable for different types of landslides, so monitoring data of different types of landslides must be distinguished. However, due to the disturbance of external influencing factors, the deformation curve will eventually deviate from the ideal curve.

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If the landslide is affected by nonperiodic factors e. Under the influence of periodic factors e. In addition, the cumulative displacement may remain at a similar level due to the stable state of landslides or errors in the monitoring process. The monitoring data was gathered from the archives of the Institute of Geological Environment Monitoring in Yunyang County.

So the deformations of landslides are creep 41 , In addition, it should be noted that for very slow and extremely slow landslides, monthly displacement data can be considered detailed enough. As seen in Fig. Sometimes due to the result of accidental errors or spatial inhomogeneity of landslide deformation, different types of displacement curves may appear at different monitoring points on the same landslide. However, a study regarding landslide rainfall warnings should primarily focus on landslide movements during or after rainfall events.

It is not practical to incorporate landslide displacement data into statistical samples without significant accelerated deformation. Therefore, to eliminate the disturbance of landslides with stable deformation, statistical samples with similar deformation characteristics are first selected from each landslide.

The principles for selection require obvious deformation trend of monitoring data in recent years. Meanwhile, considering the systematic errors associated with GPS equipment, the monitoring points with an average annual displacement component of less than 10 mm along the main sliding direction during the entire monitoring period are eliminated.

Full size image Division of study period Rainfall and reservoir water level fluctuation are the two most important factors triggering landslide movement in the TGRA 40 , Histidine protonation states as used by Hub et al.

B Transition rates between the two minima in ubiquitin: rates from A to B left and from B to A right. Asim Panhwer. Introduction To Statistical Theory Part 1.

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