The thermal effect of groundwater flow on temperature distribution in the Sendai Plain

H. G.L.N. Gunawardhana; S. Kazama; M. Sawamoto

The thermal effect of groundwater flow on temperature distribution in the Sendai Plain

H. G.L.N. Gunawardhana, S. Kazama, M. Sawamoto

نتاج البحث: Conference contribution

ملخص

Understanding the response of aquifer thermal regime on different climatic events is important to predict the effects of climate change in groundwater aquifers. A heat transport model that incorporates the effect of groundwater flow was developed to estimate the seasonal heat flux change in the Sendai Plain. Domenico & Palciauskas's analytical solution for 2-D heat transport was used to investigate the heat flow during four months time period (From 01-May-2007 to 31-August-2007). Potential distribution of groundwater flow was simulated by means of the MODFLOW numerical code. Simulated results were verified with observed water level and temperature records at three observation wells. 47.5 mW/m² of maximum vertical heat flux was estimated near to the Nanakita River and it also noticed about 17% heat flux change during two extreme precipitation events of simulation time.

اللغة الأصلية	English
عنوان منشور المضيف	From Headwaters to the Ocean
العنوان الفرعي لمنشور المضيف	Hydrological Changes and Watershed Management - Proc. of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHAN 2008
الصفحات	329-335
عدد الصفحات	7
حالة النشر	Published - 2009
منشور خارجيًا	نعم
الحدث	International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHANGE 2008 - Kyoto, Japan المدة: أكتوبر ١ ٢٠٠٨ → أكتوبر ٣ ٢٠٠٨

سلسلة المنشورات

الاسم	From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proceedings of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCH

Other

Other	International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHANGE 2008
الدولة/الإقليم	Japan
المدينة	Kyoto
المدة	١٠/١/٠٨ → ١٠/٣/٠٨

ASJC Scopus subject areas

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???subjectarea.asjc.2300.2312???

أهداف الأمم المتحدة للتنمية المستدامة

يساهم هذا المخرج في تحقيق أهداف الأمم المتحدة للتنمية المستدامة التالية (SDGs)

الملفات والروابط الأخرى

قم بذكر هذا

Gunawardhana, H. G. L. N., Kazama, S., & Sawamoto, M. (2009). The thermal effect of groundwater flow on temperature distribution in the Sendai Plain. في From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proc. of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHAN 2008 (الصفحات 329-335). (From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proceedings of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCH).

The thermal effect of groundwater flow on temperature distribution in the Sendai Plain. / Gunawardhana, H. G.L.N.; Kazama, S.; Sawamoto, M.
From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proc. of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHAN 2008. 2009. صفحة 329-335 (From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proceedings of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCH).

نتاج البحث: Conference contribution

Gunawardhana, HGLN, Kazama, S & Sawamoto, M 2009, The thermal effect of groundwater flow on temperature distribution in the Sendai Plain. في From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proc. of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHAN 2008. From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proceedings of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCH, الصفحات 329-335, International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHANGE 2008, Kyoto, Japan, ١٠/١/٠٨.

Gunawardhana HGLN, Kazama S, Sawamoto M. The thermal effect of groundwater flow on temperature distribution in the Sendai Plain. في From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proc. of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHAN 2008. 2009. صفحة 329-335. (From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proceedings of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCH).

Gunawardhana, H. G.L.N. ; Kazama, S. ; Sawamoto, M. / The thermal effect of groundwater flow on temperature distribution in the Sendai Plain. From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proc. of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHAN 2008. 2009. الصفحات 329-335 (From Headwaters to the Ocean: Hydrological Changes and Watershed Management - Proceedings of the International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCH).

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abstract = "Understanding the response of aquifer thermal regime on different climatic events is important to predict the effects of climate change in groundwater aquifers. A heat transport model that incorporates the effect of groundwater flow was developed to estimate the seasonal heat flux change in the Sendai Plain. Domenico & Palciauskas's analytical solution for 2-D heat transport was used to investigate the heat flow during four months time period (From 01-May-2007 to 31-August-2007). Potential distribution of groundwater flow was simulated by means of the MODFLOW numerical code. Simulated results were verified with observed water level and temperature records at three observation wells. 47.5 mW/m2 of maximum vertical heat flux was estimated near to the Nanakita River and it also noticed about 17% heat flux change during two extreme precipitation events of simulation time.",

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author = "Gunawardhana, {H. G.L.N.} and S. Kazama and M. Sawamoto",

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AU - Gunawardhana, H. G.L.N.

AU - Kazama, S.

AU - Sawamoto, M.

PY - 2009

Y1 - 2009

N2 - Understanding the response of aquifer thermal regime on different climatic events is important to predict the effects of climate change in groundwater aquifers. A heat transport model that incorporates the effect of groundwater flow was developed to estimate the seasonal heat flux change in the Sendai Plain. Domenico & Palciauskas's analytical solution for 2-D heat transport was used to investigate the heat flow during four months time period (From 01-May-2007 to 31-August-2007). Potential distribution of groundwater flow was simulated by means of the MODFLOW numerical code. Simulated results were verified with observed water level and temperature records at three observation wells. 47.5 mW/m2 of maximum vertical heat flux was estimated near to the Nanakita River and it also noticed about 17% heat flux change during two extreme precipitation events of simulation time.

AB - Understanding the response of aquifer thermal regime on different climatic events is important to predict the effects of climate change in groundwater aquifers. A heat transport model that incorporates the effect of groundwater flow was developed to estimate the seasonal heat flux change in the Sendai Plain. Domenico & Palciauskas's analytical solution for 2-D heat transport was used to investigate the heat flow during four months time period (From 01-May-2007 to 31-August-2007). Potential distribution of groundwater flow was simulated by means of the MODFLOW numerical code. Simulated results were verified with observed water level and temperature records at three observation wells. 47.5 mW/m2 of maximum vertical heat flux was estimated near to the Nanakita River and it also noticed about 17% heat flux change during two extreme precipitation events of simulation time.

KW - Groundwater

KW - Heat flux

KW - MODFLOW

KW - Sendai Plain

KW - Temperature effect

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M3 - Conference contribution

AN - SCOPUS:79952353541

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BT - From Headwaters to the Ocean

T2 - International Conference on Hydrological Changes and Management from Headwaters to the Ocean, HYDROCHANGE 2008

Y2 - 1 October 2008 through 3 October 2008

ER -

The thermal effect of groundwater flow on temperature distribution in the Sendai Plain

ملخص

سلسلة المنشورات

Other

ASJC Scopus subject areas

أهداف الأمم المتحدة للتنمية المستدامة

الملفات والروابط الأخرى

بصمة

قم بذكر هذا