Hydrogeo parameter - Revision history

DanielS at 21:02, 21 November 2012

2012-11-21T21:02:23Z

← Older revision		Revision as of 21:02, 21 November 2012
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		+	[[pt:Parâmetro_Hidrogeológico]]
	It is assumed that the storage capacity and storage coefficient of the upper ground water storage are lower than the lower one. This is so due to the fact that the storage in the lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.		It is assumed that the storage capacity and storage coefficient of the upper ground water storage are lower than the lower one. This is so due to the fact that the storage in the lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.

DanielS at 21:00, 21 November 2012

2012-11-21T21:00:51Z

← Older revision		Revision as of 21:00, 21 November 2012
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	A sample parameter file for different geological formations of Thuringian catchment is provided as a example.		A sample parameter file for different geological formations of Thuringian catchment is provided as a example.

−	After setting up the model file, ~~users~~ may wish to change the values (storage and recession coefficient) and observe their influence on hydrographs. This might provide ideas about the sensitivity of these values in model results.	+	After setting up the model file, you may wish to change the values (storage and recession coefficient) and observe their influence on hydrographs. This might provide ideas about the sensitivity of these values in model results.

DanielS at 21:00, 21 November 2012

2012-11-21T21:00:07Z

← Older revision		Revision as of 21:00, 21 November 2012
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	[[File:Hydro-geo.png\|Table hydro-geo parameter]]		[[File:Hydro-geo.png\|Table hydro-geo parameter]]

−	A sample parameter file for different geological formations of ~~Thurigian~~ catchment ~~are~~ provided as a example.	+	A sample parameter file for different geological formations of Thuringian catchment is provided as a example.

	After setting up the model file, users may wish to change the values (storage and recession coefficient) and observe their influence on hydrographs. This might provide ideas about the sensitivity of these values in model results.		After setting up the model file, users may wish to change the values (storage and recession coefficient) and observe their influence on hydrographs. This might provide ideas about the sensitivity of these values in model results.

DanielS at 20:56, 21 November 2012

2012-11-21T20:56:28Z

← Older revision		Revision as of 20:56, 21 November 2012
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	It is assumed that the storage capacity and storage coefficient of the upper ground water storage are lower than the lower one. This is so due to the fact that the storage in the lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.		It is assumed that the storage capacity and storage coefficient of the upper ground water storage are lower than the lower one. This is so due to the fact that the storage in the lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.

−	Schwarze (1999) provides recession constants and volumes of the lower ground water storage for ~~differernet~~ types of hydrogeological formations (Figure below). The information provided on this publication could be very instrumental in deriving the parameters values of a catchment for users.	+	Schwarze (1999) provides recession constants and volumes of the lower ground water storage for different types of hydrogeological formations (Figure below). The information provided on this publication could be very instrumental in deriving the parameters values of a catchment for users.

	[[File:Hydro-geo.png\|Table hydro-geo parameter]]		[[File:Hydro-geo.png\|Table hydro-geo parameter]]

DanielS at 20:36, 21 November 2012

2012-11-21T20:36:57Z

← Older revision		Revision as of 20:36, 21 November 2012
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−	It is assumed that the storage capacity and storage coefficient of the upper ground water storage are lower than the lower ~~ground water storage~~. It is ~~because~~ the storage in lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.	+	It is assumed that the storage capacity and storage coefficient of the upper ground water storage are lower than the lower one. This is so due to the fact that the storage in the lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.

	Schwarze (1999) provides recession constants and volumes of the lower ground water storage for differernet types of hydrogeological formations (Figure below). The information provided on this publication could be very instrumental in deriving the parameters values of a catchment for users.		Schwarze (1999) provides recession constants and volumes of the lower ground water storage for differernet types of hydrogeological formations (Figure below). The information provided on this publication could be very instrumental in deriving the parameters values of a catchment for users.

DanielS at 20:34, 21 November 2012

2012-11-21T20:34:56Z

← Older revision		Revision as of 20:34, 21 November 2012
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−		+	It is assumed that the storage capacity and storage coefficient of the upper ground water storage are lower than the lower ground water storage. It is because the storage in lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.
−	It is assumed that the storage capacity and storage coefficient of the ~~uppper~~ ground water storage are lower than the lower ground water storage. It is because the storage in lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.	+

	Schwarze (1999) provides recession constants and volumes of the lower ground water storage for differernet types of hydrogeological formations (Figure below). The information provided on this publication could be very instrumental in deriving the parameters values of a catchment for users.		Schwarze (1999) provides recession constants and volumes of the lower ground water storage for differernet types of hydrogeological formations (Figure below). The information provided on this publication could be very instrumental in deriving the parameters values of a catchment for users.

Santosh: Created page with " It is assumed that the storage capacity and storage coefficient of the uppper ground water storage are lower than the lower ground water storage. It is because the storage in lo..."

2012-09-28T16:40:52Z

Created page with " It is assumed that the storage capacity and storage coefficient of the uppper ground water storage are lower than the lower ground water storage. It is because the storage in lo..."

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It is assumed that the storage capacity and storage coefficient of the uppper ground water storage are lower than the lower ground water storage. It is because the storage in lower zone represents the saturated groundwater aquifer with longer residential times. These values are difficult to acquire as they cannot be directly measured.

Schwarze (1999) provides recession constants and volumes of the lower ground water storage for differernet types of hydrogeological formations (Figure below). The information provided on this publication could be very instrumental in deriving the parameters values of a catchment for users.

[[File:Hydro-geo.png|Table hydro-geo parameter]]

A sample parameter file for different geological formations of Thurigian catchment are provided as a example.

After setting up the model file, users may wish to change the values (storage and recession coefficient) and observe their influence on hydrographs. This might provide ideas about the sensitivity of these values in model results.