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  15. 635

    The Prevalence and Determinants of Stunting among Children 6 - 59 Months of Age in One of the Sub-Counties in the Rwenzori Sub-Region, Western Uganda by Enos Mirembe, Masereka, Arthur, Kiconco, Edson, Katsomyo, Clement, Munguiko

    Published 2020
    “…In this study, we established the prevalence and determinants of stunting in one of the sub-counties in this region. Methods: This was a cross-sectional descriptive study conducted in one of the sub-counties in the Rwenzori sub-region, Western Uganda from May 26th to June 26th, 2018. …”
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  16. 636

    Analyzing the geomorphometric changes of Dana County due to the Sisakhat earthquake using the Differential Synthetic Aperture Radar Interferometry (D-InSAR) method. by Sayyd Morovat Eftekhari

    Published 2024-09-01
    “…The purpose of this research is to measure the geomorphometric changes caused by the earthquake of 17th February 2021 at the level of Dana County using the radar technique differential SAR Interferometry. …”
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  17. 637

    Analysis of Landslide Motion Characteristics Based on UDEC: A Case Study of the Landslide in Shiban Village,Ganlong Town,Songtao County, Guizhou Province by LU Bifeng, ZHANG Hui, XIE Peihong

    Published 2023-01-01
    “…On July 8,2020,a landslide occurred in Shiban Village,Ganlong Town,Songtao County,Guizhou Province,causing casualties and diverting the river below.Through field investigation and section measurement,the development characteristics and formation mechanism of the landslide are analyzed.In addition,the motion characteristics of the landslide are simulated by the discrete element program UDEC to restore the deformation and failure process of the landslide from start-up to river blocking.The time-effect displacement curves of different parts of the landslide are obtained.The conclusions are as follows:The landslide is produced under the comprehensive action of unfavorable topography and geomorphology and formation lithology combination,rock mass structure,rainfall,and human engineering activities.The sliding surface is the contact surface of marlstone and coarse-grained limestone.The formation process of the landslide can be divided into three stages:leading-edge slip-trailing-edge crack,whole slippage,and collision accumulation.The landslide has a violent starting effect,and the maximum start-up rate can reach 5.24 m/s.The displacement and deformation rates of the trailing edge lag behind those of the leading edge,and the maximum horizontal displacement of the landslide is 217.5 m.…”
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    A spatial analysis of villagers\' satisfaction with services provided by Rural Water and Wastewater Company (A case study of Fazl Dehestan, Neyshabur County) by Hamdollah Sojasi qidari, Hamide Mahmoodi, Hoori havvaei

    Published 2018-03-01
    “…This study was conducted in a descriptive-analytical method, and the population was comprised of 132 households randomly selected from rural residents living in rural areas of Central District of Neyshabur County with an acceptable reliability score. Investigating the relationship between the five dimensions of the study and the individual characteristics indicates that there is a significant relationship between age, gender and education level and satisfaction with quality of the services in sample villages. …”
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  20. 640

    A pilot study of dimeticone oils versus sodium carbonate treatment for tungiasis: A randomized cohort trial in Homa Bay County, Kenya. by Kana Suzuki, Yasuhiko Kamiya, Chris Smith, Satoshi Kaneko, Gordon Okomo, Asiko Ongaya, Evans Amukoye

    Published 2024-07-01
    “…This study evaluated the 7-day cure rates for tungiasis by comparing sodium carbonate and NYDA treatments in Homa Bay County, Kenya.<h4>Methodology/principal findings</h4>This was a randomized, observer-blinded, parallel-treatment cohort trial. …”
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