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Vol.52, No.3, PP.121-183
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1
Applying Portable Drilling Equipment to Explore the Characteristics of Surface Runoff and Shallow Groundwater along a Gully in a Natural Forest
52(3):121-134
Wei-Chen Hsiao Wei-Li Liang*
* Corresponding Author. E-mail : liangwl@ntu.edu.tw
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2
From Exploring the Source of the Rziha Formula to Evaluating Time of Concentration
52(3):135-144
Yen-Shuo Huang[1] Chia-Ning Yang[2] Ching-Ying Tsou[3] Su-Chin Chen[4]*
* Corresponding Author. E-mail : scchen@nchu.edu.tw
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3
Assessment of Probability of Failure on Rainfall-Induced Shallow Landslides Using a Fuzzy Point Estimate Method
52(3):145-157
Ya-Sin Yang[1] Hsin-Fu Yeh[1]* Chien-Chung Ke[2] Nai-Chin Chen[2] Kuo-Chin Chang[3]
* Corresponding Author. E-mail : hfyeh@mail.ncku.edu.tw
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4
Assessment of the Potential of Groundwater Quality Indicators by Geostatistical Methods in Semi-arid Regions
52(3):158-167
Mobin Eftekhari [1]* Seyed Ahmad Eslaminezhad [2] Mohammad Akbari [3] Yashar DadrasAjirlou [4] Ali Haji Elyasi [5]
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Assessment of the Potential of Groundwater Quality Indicators by Geostatistical Methods in Semi-arid Regions
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Mobin Eftekhari [1]* Seyed Ahmad Eslaminezhad [2] Mohammad Akbari [3] Yashar DadrasAjirlou [4] Ali Haji Elyasi [5]

Abstract
Conducting groundwater quality studies is a practical necessity for obtaining quality information from water resources. Corrosion and sedimentation are important characteristics and quality indicators of groundwater. The
purpose of this study is to analyze the geostatistical potential of corrosion and sedimentation of groundwater as important indicators of aquifer quality in semi-arid regions such as Birjand plain. For this purpose, 27 wells were sampled and geostatistical analyzes were performed by kriging geostatistical method. The results showed that all qualitative components follow the spherical variogram model. The range of effect of the measured indices was from 3220 m (RSI)to 10300 m (TH). The range of effect of LSI and RSI is smaller than the range of effect of their components and looks similar. Due to the inverse relationship between the Rayznr index and the Langelier index, in the western and southwestern parts of the aquifer where the value of the Langelier index and corrosion potential are minimal, in this part of the aquifer the indices are maximum. Also, in the southeast and east of the aquifer, the pH and in the southwest of the aquifer alkalinity is higher than other parts of the aquifer. Due to the direct relationship between the Langelier index and pH, TDS, alkalinity and hardness, the spatial distribution of the LSI index is similar to the distribution of these components and follows a similar trend. In other words, it can be said that the average Langelier index for Birjand plain indicates its corrosion.
Key Words: Langelier index, corrosion, sedimentation, Birjand plain.
〔1〕Civil Engineering, Water and Hydraulic Structures, Young Researchers and Elite Club, Mashhad Branch, Islamic Azad University, Mashhad,Iran
〔2〕Department of surveying and Geomatics Engineering, College of Engineering, University of Tehran, Tehran, Iran
〔3〕Department of Civil Engineering, University of Birjand, Birjand, Iran
〔4〕Water engineering and resources management, department of water engineering and hydraulic structures, faculty of civil engineering, Semnan University, Semnan, Iran
〔5〕Water and Hydraulic Structures, Department of Civil Engineering, science and research Branch, Islamic Azad University, Tehran, Iran
* Corresponding Author. E-mail :
Received: 2020/10/26
Revised: 2021/01/12
Accepted: 2021/02/22
5
Impacts of Conservation Tillage and Crop Residue Management on Soil Properties: A Short-Term Trial in Iran
52(3):168-175
Sakineh Mazdarani [1]* Mostafa Karimian Eghbal [2]
* Corresponding Author. E-mail : s_mazdarani@modares.ac.ir
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6
Using the Geo-Spatial Interface for WEPP to Simulate Erosion and Deposition of Sediments in the Nanhua Reservoir Watershed
52(3):176-183
Chin-Shou Lin[1]* Hsing-Chuan Ho[1] Bor-Shiun Lin[1] Je-Yi Jhang[2] Ming-Fa Tsai[2] Po-Tsung Kao[2]
* Corresponding Author. E-mail : orin@sinotech.org.tw
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