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Statements

Subject Item
n2:RIV%2F00216224%3A14310%2F10%3A00042705%21RIV11-MSM-14310___
rdf:type
skos:Concept n16:Vysledek
dcterms:description
natural groundwater flow pattern will be partly restored. Re-established groundwater flow system will be associated with an increase of groundwater discharge into draining rivers and streams. Since the groundwater inflows to streams can be contaminated by the mine water, the groundwater drainage characteristic of fractured aquifer should be carefully identified. Several methods of groundwater discharge zones identification were used including morphological analysis, thermometry, and electrical conductivity (EC) measurements. Stream temperatures and EC at more than 700 points in the area covering about 85 km2 were measured. The measurements were performed during winter period, when stream discharges were low and there was a maximum temperature contrast. There was a frequent presence of preferential discharge zones with resulting anomalous temperatures and electric conductivity values of stream water. natural groundwater flow pattern will be partly restored. Re-established groundwater flow system will be associated with an increase of groundwater discharge into draining rivers and streams. Since the groundwater inflows to streams can be contaminated by the mine water, the groundwater drainage characteristic of fractured aquifer should be carefully identified. Several methods of groundwater discharge zones identification were used including morphological analysis, thermometry, and electrical conductivity (EC) measurements. Stream temperatures and EC at more than 700 points in the area covering about 85 km2 were measured. The measurements were performed during winter period, when stream discharges were low and there was a maximum temperature contrast. There was a frequent presence of preferential discharge zones with resulting anomalous temperatures and electric conductivity values of stream water.
dcterms:title
Determination of potential mine water discharge zones in crystalline rocks at Rozna, Czech Republic Determination of potential mine water discharge zones in crystalline rocks at Rozna, Czech Republic
skos:prefLabel
Determination of potential mine water discharge zones in crystalline rocks at Rozna, Czech Republic Determination of potential mine water discharge zones in crystalline rocks at Rozna, Czech Republic
skos:notation
RIV/00216224:14310/10:00042705!RIV11-MSM-14310___
n3:aktivita
n14:Z n14:S
n3:aktivity
S, Z(MSM0021622412)
n3:cisloPeriodika
6
n3:dodaniDat
n7:2011
n3:domaciTvurceVysledku
n4:7831102 n4:8747288 n4:4371003
n3:druhVysledku
n17:J
n3:duvernostUdaju
n13:S
n3:entitaPredkladatele
n10:predkladatel
n3:idSjednocenehoVysledku
253791
n3:idVysledku
RIV/00216224:14310/10:00042705
n3:jazykVysledku
n6:eng
n3:klicovaSlova
Impact of mining - Stream thermometry - Crystalline rocks - Groundwater flow - Discharge characteristics
n3:klicoveSlovo
n15:Impact%20of%20mining
n3:kodStatuVydavatele
CZ - Česká republika
n3:kontrolniKodProRIV
[F519C39E4D03]
n3:nazevZdroje
Environmental Earth Sciences
n3:obor
n12:DB
n3:pocetDomacichTvurcuVysledku
3
n3:pocetTvurcuVysledku
4
n3:rokUplatneniVysledku
n7:2010
n3:svazekPeriodika
60
n3:tvurceVysledku
Říčka, Adam Šráček, Ondra Zeman, Josef Kuchovský, Tomáš
n3:zamer
n18:MSM0021622412
s:issn
1866-6280
s:numberOfPages
13
n5:organizacniJednotka
14310