Spring of water Prusik - Prusikuv pramen EarthCache

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Spring of water Prusik

Peat bogs sulfur springs.
 
Prusikuv Source: Mineral dioxide and water with a pleasant taste with a little sulfurhydrogen smell, temperature 9.9 ° C.
Drinking pavilion in the spa park.
Konstantinovy Lazne rightfully claim the sites of the Pilsen Region, often on a quiet unspoilt countryside civilization is rife acidulous mineral springs. Find here a number of historical monuments and interesting places, which will allow us to follow the trail of man from prehistoric times through the Middle Ages to the present.
Spa itself is situated in a beautiful park, an assortment of species naturally follow-up on the surrounding nature. The village found 35 km west of Plzen where we head towards the Karlovy Vary in the average altitude of 520 m in one of the ecologically cleanest regions of Bohemia. With a total of 932 inhabitants one of the smaller spa towns in the Czech Republic, offering a quiet family environment for its visitors.
Spa services are mainly focused on a comprehensive diagnosis, prevention and treatment of cardiovascular diseases. The main therapeutic methods in Konstantinovych Laznich are based on the medicinal use of natural resources - mineral carbonated water. Source of natural iron bicarbonate sodium-magnesium  hypotonic mineral water from a depth of 40 m has a yield of 120 to 150 liters per minute at a temperature of 9.1 o C and has the highest content of carbon dioxide in the Czech Republic.
The content of free carbon dioxide in the water here is actually the highest in the Czech Republic (3638.0 mg / l).

USE OF RESOURCES

Receivers vrt BV 11 - Prusík
BV 11 - 9.9 to 5.26 - 29.54 to 35.45 - 14.67-3136
Proclaimed as a source of natural healing source decree MZ is situated in the spa park in the previous five original Jimani spring. It is 40 meters deep with a getup: 18.5 meters in earthenware pipes 450/350 mm perforation of hl.10 m from 18.5 m to 40m then ANTICORO casing diameter of 216 mm with a perforation.
Receivers vrt BV 12 - Kokasicky
BV 12 - 8.8 to 5.29 - 49.91 to 16.07 - 31.81-2756
Proclaimed as a source of natural healing source decree MZ. It is situated in the area of the former Kokasickeho spring in the valley Polzickeho stream about 1 km west of the village. Depth 40 m deep with a getup: 18.5 meters in earthenware pipes 450/350 mm perforation of hl.10 m from 18.5 m to 40m then ANTICORO casing diameter of 216 mm with a perforation.
Source - Temperature - pH - Fe mg / l - Cl mg / l - SO4 mg / l - CO2 mg / l

Classification:
Natural, cold, simple, hypotonic, ferrous mineral water, hydrogen-carbonate-sodium-magnesium type with an increased content of silicic acid.

GEOLOGY,  TECTONICS AND HYDROGEOLOGY, TERRITORY

Thermal springs Konstantinovy Lazne complex in northwestern tip Tepelska-barandienske field at an altitude of about 520 m above sea level in places where Tepelska Flatbed pass to the southeast in the lower Stribrsko Hills. The emergence of thermal springs is the result of favorable ratio and the presence of tectonic mladotretihorniho volcanism. For the overall landscape is characteristically area parovinny relief with shallow trough zahloubenymi depression, which contrasts with the deeply incised valleys greater flow.
Around peneplain emerge from the vital heights neovulkan (Krasikov 629 m , Sheep hill, 696 m,  Hradistsky hill 632m).

GEOLOGYCAL TERRITORY

Main geological unit is algonkium and a slight flush far as is rock permokarbonskeho old. The main building materials territory Phyllite (complex chloriticko-sericitickych Phyllite with quartz veins) and a series of roof slates and spilitove series. Rock base is mostly effloresced. Color solid rock is usually gray-green and gray. Color depends mainly on the content grafit pigment. The predominant rock is Tectonics territory
From the tectonic point of view, the Board violated fylitovy complex disorders of various directions. Directions of gradients (about 70 80 °) vrstnatosti then explained hydrogeological survey in 1665 - 1969. The predominant direction of the main faults are S - J (so-called polzicka - nejvyznamejssi disorder width from several meters to tens of meters) V - Z (so-called Konstantinolazensko disorder Pricna the polzickou, takes place over Lazenska sources and end the polzicke breakdown) SV - JZ (old space Lazni). As the main tectonic nodes showed areas measured in borehole BV 12, BV 11 space at a former spa spring and the node north of railroad tracks in places where they intersect Lazenska disorder with a direction line SV - south-west, passing through the area of borehole BV 12th This third node has only theoretical meaning, and so far, without detailed investigated. In the direction of the main tectonic line from north to south flows celivsky and Polzicky stream of flowing mineral water board, whose catchment (consisting fylitickymi rocks) is virtually impermeable.

HYDROGEOLOGICAL CONDITIONS

Rocks algon old is her character for water impermeable. For hydrogeological conditions is therefore essential tectonics of the territory, which allowsleak circulation groundwater. Most active circulation is logically allowed on the tectonic lines whose prostnost is linked with the degree of fissured. Spreading rate fissure spring is here quite small ranging from 0.2 l / sec. and of 0.5 l / sec.
Great majority of failures allows output of mineral water. Band of creation is at a depth of 50 to 100 m, sometimes more. Prosta underground water soaking into the cracks, descends after them in depth here, and mixes with the juvenile carbon dioxide, water, which proplyni vodu.Proplynena water then has a greater ability to pick up from the surrounding rocks and mineral component performs better on the surface.
According to the basic genetic sorting of mineral springs Constantine Lazne awards between mainland melc spring with two thermal springs and mineral water circulation etapovym (descending, ascending). Konstantinolázensko mineral water have a relatively small mineralisaci from 300 to 1100mg / l, high levels of free CO2 of about 2500 mg / l (and 3000 mg / l), high content of iron and 60 mg / l. According to the composition belongs to the naked cold kyselkam.
After the page climatic surroundings Constantine Lazni belongs to semi-arid areas with average annual rainfall from 500 to 650 mm. It is caused mainly by affecting the cell precipitation shadow of the foothills of the Bohemian Forest and Doupovské mountains.

SURVEY TERRITORY

Be explored territory we could date back to 17th interface and 18 century, which dates back to the survey work in the vicinity Bezdruzice a curve. They are however unconfirmed. Serious polls begin, however, and in the 19 century, when it was made F.V. Hochstelterem basic geological mapped area. In 1913, the geological structure territory deals R. Kettner. More detailed survey is the subject between 1946 and 1948-51. Complete hydrogelogicky probing took place between 1962 - 1965 Stage I, which was to survey the character of the search should examine hydrogeological conditions, identify opportunities in existing geyser base and propose a new mineral water in the catchment. On the basis of favorable results was carried out between 1965 - 1969 II. stage. She had to specify thermal springs as a whole, its geological and hydrogeological conditions and clarify some details from the previous stage. By the investigation was, inter alia, to implement a number of exploratory and two catch-the borehole (BV 11 and BV 12). The work carried out but was not possible to establish infiltration territory. It is assumed that the catchment basin consists Celivskeho and Polzickeho Creek area of 12.3 km2.

QUESTIONS:

1st Photo coordinates - OPTIONAL
2nd The year of the fountain
3rd In what depth of the hole located
4th Carbon dioxide content in water
5th how big is this area?

CZ:

Prusikuv pramen

Raseliniste se sirnymi prameny.

Prusikuv pramen: Mineralni uhlicita voda s prijemnou chuti s nepatrnym sirovodikovym pachem, teplota 9,9°C.
V pitnem pavilonu v lazenskem parku.
Konstantinovy Lazne pravem nalezi k vyznamnym mistum Plzenskeho kraje, klidne o mnohdy civilizaci jeste nedotcene krajiny prosycene vyvery mineralnich kyselek. Nalezneme zde radu historickych pamatek a zajimavych mist, ktere nam dovoli sledovat stopu cloveka od praveku pres stredovek az po soucasnost.
Samotne lazenske misto je citlive zasazene do krasneho druhove pestreho lesoparku prirozene navazujiciho na okolni prirodu. Obec nalezneme 35 km zapadne od Plzne vydameli se smerem na Karlovy Vary v prumerne nadmorske vysce 520 m v jedne z ekologicky nejcistsi oblasti cech. S celkem 932 obyvateli patri mezi mensi lazenska mista v ceske republice nabizejici klidne rodinne prostredi pro sve navstevniky.
Lazenske sluzby jsou zde zamereny predevsim na komplexni diagnostiku, prevenci a leceni chorob kardiovaskularniho systemu. Hlavni lecebne metody v Konstantinovych Laznich jsou zalozeny na vyuziti prirodnich lecivych zdroju - mineralni uhlicite vody. Pramen prirodni zeleznate hydrogenuhlicitanove sodnohorecnate hypotonicke kyselky z hloubky 40 m ma vydatnost 120 - 150 l za minutu pri teplote 9,1 o C a ma nejvyssi obsah oxidu uhliciteho v cele ceske republice.
Obsah volneho oxidu uhliciteho ve zdejsi vode je skutecne vubec nejvyssi v cele ceske republice (3638,0 mg/l).

Vyuzivane zdroje

Jimaci vrt BV 11 – Prusik
BV 11 - 9,9 - 5,26 - 29,54 - 35,45 - 14,67 - 3136
Prohlasen za zdroj prirodni lecivy zdroj vyhlaskou MZ Je situovan v lazenskem parku v miste predchoziho jimani puvodnich peti pramenu. Je 40m hluboky svystroji: do 18,5 m kameninove roury 450/350 mm s perforaci od hl.10 m, od 18,5 m do 40m pak anticoro paznice o prumeru 216 mm s perforaci.
Jimaci vrt BV 12 – Kokasicky
BV 12 - 8,8 - 5,29 - 49,91 - 16,07 - 31,81 - 2756
Prohlasen za zdroj prirodni lecivy zdroj vyhlaskou MZ. Je situovan v prostoru byvaleho Kokasickeho pramene v udoli Polzickeho potoka cca 1 km zapadne od obce. Hloubka 40 m hluboky s vystroji: do 18,5 m kameninove roury 450/350 mm s perforaci od hl.10 m, od 18,5 m do 40m pak anticoro paznice o prumeru 216 mm s perforaci.
Zdroj - Teplota - pH - Fe mg/l - Cl mg/l - SO4 mg/l - CO2 mg/l
Klasifikace:
Prirodni, studena, prosta, hypotonicka, zeleznata kyselka, hydrogen-uhlicitano-sodno-horecnateho typu se zvysenym obsahem kyseliny kremicite.

Geologie, tektonika a hydrologie uzemi

Zridelni struktura Konstantinovych Laznich lezi v severozapadnim vybezku komplexu tepelsko-barandienske oblasti ve vysce okolo 520 m n.m. v mistech, kde Tepelska plosina prechazi na jihovychod do nizsi stribrske pahorkatiny. Vznik zridelni struktury je vysledkem priznivych tektonickych pomeru a pritomnost mladotretihorniho vulkanismu. Pro celkovy raz krajiny je charakteristicky plochy parovinny relief s melce zahloubenymi udolnimi depresemi, ktery kontrastuje s hluboce zariznutymi udolimi vetsich toku.
V okoli vystupuji z paroviny vyznamne kopce neovulkanitu (Krasikov 629 m n.m., Ovci vrch 696 m n.n., Hradistsky vrch 632 m n.m. atd).

Geologicka stavba uzemi

Hlavni geologickou jednotkou je algonkium a v nepatrnem plosnem rozsahu rovnez horniny permokarbonskeho stari. Hlavnim stavebnim materialem uzemi jsou fylity (komplex chloriticko-sericitickych fylitu s zilkami kremene) a to serie pokryvacskych bridlic a serie spilitove. Skalni podklad je vetsinou zvetraly. Barva pevne horniny je vetsinou sedozelene az sede barvy. Zbarveni zavisi predevsim na obsahu grafitickeho pigmentu. Prevladajici horninou je Tektonika uzemi.
Z tektonickeho hlediska je tento fylitovy komplex porusen radou poruch nejruznejsich smeru. Smery o sklony (asi 70-80o) vrstnatosti pak upresnil hydrogeologicky pruzkum v letech 1665 – 1969. Prevladajici smery hlavnich poruch jsou S – J ( tzv. polzicka – nejvyznamejssi porucha, sirka od nekolika metru az do desitek metru) V – Z ( tzv. konstantinolazenska porucha, pricna na polzickou,probiha pres lazenske prameny a konci na polzicke poruse) SV-JZ (prostor Starych Lazni). Jako hlavni tektonicke uzly se pri mereni projevily prostory u vrtu BV 12, prostor u BV 11 a byvalych lazenskych pramenu a uzel severne od zeleznicni trate v mistech kde se protinaji lazenska porucha s linii smeru SV – JZ, prochazejici prostorem vrtu BV 12. Tento treti uzel ma jen teoreticky vyznam a je zatim bez podrobnejsiho prozkoumani. Ve smeru hlavni tektonicke linie od severu k jihu proteka celivsky a Polzicky potok z radou vyveru kyselky, jehoz povodi (tvoreno fylitickymi horninami) je prakticky nepropustne.

Hydrogeologicke pomery


Horniny algonkickeho stari jsou svym charakterem pro vodu nepropustne. Pro hydrogeologicke pomery ma proto zasadni vyznam tektonika uzemi,ktere umoznuji puklinovy obeh spodni vody. Nejaktivnejsi obeh je tak logicky umoznen na tektonickych liniich, jejichz prostnost je spjata se stupnem rozpukani. Vydatnost puklinovych pramenu je zde pomerne mala od 0,2 l/sec. az po 0,5 l/sec.Prevazna vetsina poruch umoznuje vystup mineralnim vodam. Pasmo jejich tvoreni je v hloubce 50 – 100 m, misty i vice. Prosta podzemni voda se vsakuje do puklin, sestupuje po nich do hloubky a zde se smesuje s juvenilnim kyslicnikem uhlicitym, ktery vodu proplyni vodu.Proplynena voda pak ma vetsi schopnost prejimat z okolnich hornin mineralni slozky a lepe vystupuje k povrchu.
Podle zakladniho genetickeho trideni mineralnich zridel nalezi Konstantinovy Lazne mezi kontinentalni zridla s melci zridelni strukturou a dvou etapovym obehem mineralni vody (sestupna, vzestupna).Konstantinolazenske kyselky maji pomerne malou mineralisaci od 300 do 1100mg/l, vysoky obsah volneho CO2 okolo 2500 mg/l (i 3000 mg/l), vysoky obsah zeleza az 60 mg/l. Podle slozeni patri k studenym prostym kyselkam.
Po strance klimaticke patri okoli Konstantinovych Lazni k polosuchym oblastem s prumernym rocnim uhrnem srazek 500 – 650 mm. Je to zpusobeno predevsim ovlivnenim cele oblasti srazkovym stinem predhuri ceskeho lesa a Doupovskych hor


Pruzkum uzemi


Zahajeni pruzkumu uzemi by jsme mohli datovat na rozhrani 17. a 18. stoleti, na kdy se datuji kutaci prace v okoli Bezdruzic a Krivcu. Ty jsou vsak nepotvrzene. Seriozni pruzkumy zacinaji vsak az v polovine 19. stoleti, kdy bylo provedeno F.V. Hochstelterem zakladni geologicke zmapovani oblasti. V roce 1913 se geologickou stavbou uzemi zabyva R.Kettner. Podrobnejsimu pruzkumu je oblast podrobena v letech 1946 a 1948-51. Kompletni hydrogelogicky pruzkum pak probehl v letech 1962 – 1965 I. etapou, ktera mela charakter vyhledavaciho pruzkumu mela overit hydrogeologicke pomery, zjistit moznosti stavajici zridelni zakladny a navrhnout novy zpusob jimani mineralnich vod. Na zaklade priznivych vysledku byla provedena v letech 1965 – 1969 II. etapa. Ta mela za ukol upresnit zridelni strukturu jako celek, jeji geologicke a hydrogeologicke pomery a upresnit nektere detaily z predchozi etapy. Soucasti pruzkumu bylo mimo jine i provedeni cele rady pruzkumnych a dvou jimacich vrtu (BV 11 a BV 12). Z provedenych praci nebylo vsak mozne presne stanovit infiltracni uzemi. Predpoklada se, ze infiltracni oblast je tvorena povodim celivskeho a Polzickeho potoka o rozloze 12,3 km2.

Otazky:

1. Foto na souradnicich
2. Letopocet na fontane
3. V jake hloubce se nachazi vrt
4. Obsah oxidu uhliciteho ve vode
5. Na jake rozloze se nachazi tato oblast ?

Ha, pocítadlo zjistilo, jsi kacer, ktery zrovna brejli na moji kesku. Dik