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Spatial Strategies for Crowd Management in Haridwar, India 印度哈里瓦尔人群管理的空间策略
Pub Date : 2019-07-27 DOI: 10.23953/CLOUD.IJACEAR.421
Sindhuja Kasthala, B. Binoy, H. S. Lakra
Crowd-related hazards are prevalent in densely populated countries like India where there is increase in the number of visitors to religious gatherings (NDMA, 2014) and the major task of authorities lies in reducing the risk of crowd disasters. The purpose of this work is to spatially analyze the crowd management and emergency preparedness strategies formulated by authorizes for the safe conduction of the Ardh Kumbh Mela, 2016 in Haridwar with the help of tools and technologies. In this paper, we examine the potential of using technologies like Remote Sensing and Geographical Information System (GIS) for evaluating and recommending guidelines for crowd management and emergency response. The study was largely dependent on field visits during the 2016 Ardh Kumbh Mela and it attempted to capture the merits and demerits of the proposed crowd management strategies such as the major crowd flow routes, infrastructure facilities, critical crowd management and emergency routes to hospitals. Various analyses like crowd capacity analysis, infrastructure scoring, and crowd flow analysis helped to recommend guidelines for Crowd Control Management.
人群相关的灾害在印度等人口稠密的国家很普遍,那里参加宗教集会的游客数量在增加(NDMA, 2014),当局的主要任务是减少人群灾害的风险。本研究的目的是在工具和技术的帮助下,对2016年哈里瓦尔大壶节安全举办的人群管理和应急准备策略进行空间分析。在本文中,我们研究了使用遥感和地理信息系统(GIS)等技术来评估和推荐人群管理和应急响应指南的潜力。该研究在很大程度上依赖于2016年大壶节期间的实地访问,并试图了解拟议的人群管理战略的优缺点,如主要人群流动路线、基础设施、关键人群管理和前往医院的紧急路线。各种分析,如人群容量分析、基础设施评分和人群流量分析,有助于为人群控制管理推荐指导方针。
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引用次数: 0
Assessment of Dynamic Groundwater Reserve of Kamarup District Lower Assam, India 印度下阿萨姆邦Kamarup地区动态地下水储量评价
Pub Date : 2018-12-07 DOI: 10.23953/CLOUD.IJACEAR.391
A. B. Devi, A. Nair
Despite sufficient rainfall, a large portion of the northeast region of India suffers from water scarcity especially during dry seasons when groundwater acts as a significant source of water supply. Consequently, a proper assessment of groundwater condition at a district/block level is very much essential to adopt sustainable water management practices. Additionally, climate change and crossborder water disputes generate new challenges in the water management of Northeast India. In this study, an attempt has been made to present groundwater scenario of Kamarup district in lower Assam as a case study representing North-East India. For this purpose, we used the available temporal groundwater-level data derived from observation wells at five sites namely Agyathuri, Azara, Bamunigaon, Khara and Rangia located in the Kamrup district (lower Assam) of north-east India. The dynamic groundwater reserve (DGWR) has been estimated for the period from 1996 to 2006 using groundwater level data from these five sites along with monthly rainfall data and published pumping test data. This will help to analyze the groundwater dynamics of the study area. In order to cross check the obtained results, we used terrestrial water storage changes (TWS) derived from GRACE (Gravity Recovery and Climate Experiment) satellite data. TWS is a satellite-based monthly mean liquid water equivalent thickness with one degree spatial and monthly temporal resolution available from 2002. Terrestrial water storage includes the soil moisture, surface water equivalent and groundwater anomaly based on satellite observations of earth gravity field from the (GRACE). In the present study, TWS data was analyzed for over a period of 5 years from 2002 to 2006. The results of the study indicate that the maximum groundwater fluctuation was in the range of 0.84 to 3.48 m and minimum between -5.07 to -1.47m. Over the entire study area, we observed a decrease in dynamic groundwater reserves. From the trend analysis, it is obvious that there is an increasing trend of groundwater level at Khara, Rangia and Bumungiaon site and a decreasing trend at Agyathuri and Azara site. Further, the DGWR results showed that two sites (Agyathuri and Azara) were continuously subjected to stress from 1999 onwards. We observed that the DGWR and TWS are showing a comparable negative trend in the dynamic groundwater storage capacity for the study period. In the year 2004 the recorded TWS and estimated average_DGWR are relatively high during the study period. Thus, the results of this study provide a clear picture of spatial and temporal variations of dynamic groundwater resources in the study area, based on which important recommendations can Research Article IJACEAR– An Open Access Journal (ISSN 2348-5124) International Journal of Advanced Civil Engineering and Architecture Research 90 be made for managing the scarce groundwater resources of the study area in a sustainable manner to address future challenges.
尽管降雨量充足,但印度东北部的大部分地区仍然缺水,特别是在干旱季节,地下水是重要的供水来源。因此,对地区/街区一级的地下水状况进行适当评估对于采取可持续的水管理做法是非常重要的。此外,气候变化和跨境水资源争端给印度东北部的水资源管理带来了新的挑战。在本研究中,尝试将下阿萨姆邦Kamarup地区的地下水情景作为代表印度东北部的案例研究。为此,我们使用了从位于印度东北部Kamrup地区(下阿萨姆邦)的Agyathuri、Azara、Bamunigaon、Khara和Rangia五个地点的观测井中获得的现有时间地下水位数据。利用这五个地点的地下水位数据、每月降雨量数据和公布的抽水试验数据,估算了1996年至2006年的动态地下水储量。这将有助于分析研究区地下水动态。为了对得到的结果进行交叉检验,我们使用了GRACE (Gravity Recovery and Climate Experiment)卫星数据得到的陆地储水变化(TWS)。TWS是2002年以来基于卫星的月平均液态水当量厚度,具有一度空间和月时间分辨率。基于GRACE卫星地球重力场观测,陆地储水量包括土壤水分、地表水当量和地下水异常。在本研究中,TWS数据分析了2002年至2006年的5年时间。研究结果表明:地下水波动最大值为0.84 ~ 3.48 m,最小值为-5.07 ~ -1.47m。在整个研究区域,我们观察到动态地下水储量减少。从趋势分析来看,Khara、Rangia和Bumungiaon站点的地下水位有明显的上升趋势,Agyathuri和Azara站点的地下水位有下降趋势。此外,DGWR结果表明,两个站点(Agyathuri和Azara)自1999年以来持续受到压力。研究发现,在研究期内,三峡库区和TWS的动态地下水库容均呈负变化趋势。在2004年的研究期间,录得的总水量和估计的平均总水量相对较高。因此,本研究的结果为研究区地下水资源动态的时空变化提供了清晰的图像,并可在此基础上提出重要建议,以可持续的方式管理研究区稀缺的地下水资源,以应对未来的挑战。
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引用次数: 1
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International Journal of Advanced Civil Engineering and Architecture Research
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