Siva ashtothara sathanamavali in malayalam pdf

Om Sada-pancha-dashaatmaikya svarupayai namo namahWho is the Eternal Self of 15 fundamentals principles in the creation 5 senses, 5 pranas and 5 inner organs. Sri Lalitha Ashtothara Sathanamavali1. Om Janma-mrutya jaraa-roga bhanjanaayai namo namahWho eliminates birth, death, aging and disease of her devotees. Sri Lalitha Peetham cordially invites all devotees to participate in Om Padma-pashankusha-lasat-karaabjayai namo namahWho holds lotus, rope and ankusa a stick used by mahouts to control elephants in her lotus like hands.

Om Pativratangana-abeeshta phaladaayai namo namahWho fulfils the wishes of chaste women. Om Suma-banekshu-kodanda-manditaayai namo namahWho holds arrows axhtothara of flowers and bow made of sugar cane in her hands.

Om Tri-lochana krutollasa phaladaayai namo namahWho gives joy to Lord Siva. Om Virakti-bhakti vijnaana-sidhidaayai namo namahWho bestows dispassion, devotion, wisdom and fulfillment to devotees. Om Sree-shodashaksharee mantra madhyagaayai namo namahWho dwells in the 16 syllabled sacred mantra Shodhashi.

Sri Tulasi Ashtothara Shatanamavali in Telugu -? Om Taanbula-purita-smera-vadanayai namo namahWhose face is adorned with smile and mouth is filled with betal leaves. Om Raaja-raajaarchita pada-sarojaayai namo namahWhose lotus feet are worshipped by monarchs. Om Avyaja-karuna pura-puritaayai namo namahWho is full of true compassion. Om Sachaamara rama-vanee viijitayai namo namahWho is served by Goddesses Lakshmi and Saraswati with handfans.

Om Haani vrudhi gunaadhikya-rahitaayai namo namahWho ashtoghara undergoes any changes like growth, decay, etc. Om Vajra-manikya-kataka kireetayai namo namahWho is wearing bracelets and crown decorated with diamonds and rubies.

Om Bhanda-daitya maha-satma naashanaayai namo namahWho destroyed the huge mansion of the demon Bhanda. The spatial distribu- Spatial distribution tion of electrical conductivity reveals that an untreated industrial effluents, landfill and anthropogenic activities affecting their groundwater quality in its vicinity and the Introduction surrounding area.

The dominance of ions was in the order of Na? The statistical results pollutants MoWR In arid and semiarid parts of reveals that the groundwater chemistry gets altered by India, groundwater resources have condensed due to silicate weathering, ion exchange, leaching, anthropogenic vagaries in monsoons, increase in population, industriali- input from agricultural return flow and longer distance of zation, use of fertilizers and pesticides, non-adoption of migrating groundwater.

The hydrogeochemical regimes are adequate soil conservation measures, improper crop rota- distributed along the upstream side, northwestern, western tion, non-planning and management of irrigation systems and eastern parts of the study area.

The study highlights the and extraction of groundwater in excess of recharge Sri- vastava and Ramanathan , which make aquifers water stressed and most parts of India are likely to face severe water scarcity by SERI Groundwater undergoes inorganic chemical reactions as it moves through fracture zones and K. The normal annual rainfall over the study area is about ; Kvitek et al. The geology of the study area is This technique helps to simplify and organize data underlined by rocks representing metasediments of set in order to make useful generalizations and insight in Archaean age with major litho units encompassing char- water systems for reliable management of water resources nockites, granitic gneiss, calc granulites, syenite and ultra and rapid solution for pollution problems Raghunath et al.

The study area, Thirumanimuttar sub-basin, a hard rock Groundwater occurrence in the study area is mainly terrain receives major part of rainfall from northeast associated with development of secondary porosity as a monsoon. The surface water sources are generally precar- result of weathering and fissures along with development of ious to get their supply during monsoon seasons and during fractures. The distinct dry and wet season have facilitated non-monsoonal periods, people depend on groundwater deep weathered and regolith under semiarid climatic con- resources for their domestic, agricultural and industrial ditions.

The depth of weathering ranges from 2. Most of human, agricultural activities and the rest by industries the dug wells are confined to the weathered zone, while the manufacturing chemicals, paints, dying, bleaching and bus bore wells extends into the fractured zone. Water table body building which dispose industrial and hazardous reaches to 0.

Groundwater development categorized as over exploited or critical. Incidence of is by shallow open wells and deep bore wells. Materials and methods a. Excessive use of fertilizers and pesticides in agri- culture has also reportedly resulted in localized enrichment Sample preparation and analytical method of nitrate in the phreatic zone Vasanthavigar et al. In over view of the comparatively high level of ground To determine the groundwater quality and pollution sour- water development in the major part of the study area and ces a detailed study was conducted in Thirumanimuthar the quality problems due to geogenic and anthropogenic region by collecting groundwater samples for two factors the study of behavior of aquifers in the study area seasons pre monsoon PRM and post monsoon POM.

Few geochemical Each sample was collected in acid-washed polyethylene studies were carried out in the Thirumanimuttar basin by 1, ml bottle with strict adherence to the sampling pro- Vasanthavigar et al. There has been tocol as described by Gale and Robins Samples limited attempt to study the statistical nature of the were filtered using a 0.

Hence an attempt has been made membrane. The bottles were tightly capped to protect in the present study to understand the chemical character- samples from atmospheric CO2, adequately labeled, and istics of groundwater to demarcate the pollution potential preserved in the refrigerator until they were taken to the zones along with spatial and temporal variations using laboratory for measurement.

Precaution was also taken to multivariate statistical analysis. The samples were immediately transferred to the labora- tory and analyzed for major ions by employing standard Study area methods.

Chloride Cl- by standard AgNO3 titra- drainage of about 2, km2. The analytical data by reducing the numbers of dimensions without much precision for ions was determined by the ionic balances loss of information Irawan et al. The mathematical and ables axes called the principal components, which are statistical results have been commutated from statistical linear combination of the original variables Sarbu and Pop package for social sciences SPSS V17 software.

It is a way of identifying and expressing data in such a way to highlight their similarities and differences. Data treatment Factor analysis FA is a generic name given to a class of multivariate statistical methods whose primary purpose For a better understanding of the groundwater system and is data reduction and summarization. Factor analysis is chemistry, multivariate analyses can be performed using widely used statistical technique in hydrochemical research both chemical species major cations and anions and to explain the origin of groundwater chemistry Gupta and physicochemical data such as electrical conductivity, pH Subramanian The aim of factor analysis in hydro- and alkalinity Kazi et al.

Statistical method is used chemistry is to explain observed relations in terms of as an analytical tool to reduce and organize large hydro- variables called factors. These factors are neither nor chemical datasets into groups with similar characteristics. Spatial or tem- The basic purpose of such an analysis is to interpret rela- poral measurements of chemical or physical properties tionship among the variables used for classification of usually do not directly reveal the underlying governing original data set.

Main advantage of principal component processes in the groundwater system Suk and Lee In hierarchical seasons. The negative logarithm of Hydrogen ion pH cluster analysis, each case as separate cluster and joins concentration ranges from 6. In this study, HCA was performed alkaline nature of groundwater. The Higher EC was noted in Salem region indicating the pol- between groups linkage method uses analysis of variance luted nature of groundwater. Both temporal magnesium calcite and gypsum Lakshmanan et al.

This technique helps cating sources from feldspar weathering plagioclase to determine the hydrological factors such as aquifer bearing along with over exploitation of groundwater Hem boundaries, ground water flow and paths hydrochemical ; Chidambaram et al.

During PRM high aver- components, to identify the control of rock chemistry on age Compatible with iPhone, iPad and iPod touch. This App will take your mind to another level of inner peace and tranquility. Hello Gsvrao, We are not charging anything for this. Anjaneya Ashtottara Shatanamavali Laxmi Teluug Narasimha karavalamba Stotram It is difficult to transliterate Sanskrit words into English with full justification to the original sounds.

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