講演情報
[AHW32-P15]Observation for the temporal variation of lacustrine groundwater discharge (LGD) in Lake Biwa
*齋藤 光代1、小野寺 真一2、朱 爱萍2,3、友澤 裕介2、金 广哲2、伴 修平4、奥田 昇5 (1.岡山大学大学院環境生命科学研究科、2.広島大学大学院総合科学研究科、3.中山大学地理科学規画学院、4.滋賀県立大学、5.総合地球環境学研究所)
キーワード：
Lacustrine groundwater discharge、Temporal variation、Lake Biwa
Lacustrine groundwater discharge (LGD) is one of the potential nutrient paths from a catchment to a lake. Lake Biwa is the largest freshwater lake in Japan. Some researchers have pointed out the presence of LGD in littoral area of the lake. However, the temporal variation of LGD is not well evaluated in the previous studies. In the present research, we aimed to examine the temporal variation of LGD in Lake Biwa based on the results of continuous measurements at the littoral area.
We conducted the mooring observation for about 9 hours from morning to evening in July 2016. Water temperature, electric conductivity and radon (222Rn) concentration in lake water were measured at the littoral areas near Hikone city. 222Rn is a radioactive element of uranium (238U) series with 3.8 day of half-life. 222Rn is a useful tracer of groundwater discharge because it generally enriched in groundwater than surface water. We also measured flow velocity using ADCP (Acoustic Doppler Current Profiler). 222Rn concentration in lake water was totally high compared with the offshore water. It suggests the nearshore water is influenced by LGD. Water level changed about 5 cm and observed maximum velocity was ± 0.2~0.3 m3/s during the period. It indicates exchange process between nearshore water and offshore water occurred in the study area. 222Rn concentration tended to decrease with the increase of water exchange.
We conducted the mooring observation for about 9 hours from morning to evening in July 2016. Water temperature, electric conductivity and radon (222Rn) concentration in lake water were measured at the littoral areas near Hikone city. 222Rn is a radioactive element of uranium (238U) series with 3.8 day of half-life. 222Rn is a useful tracer of groundwater discharge because it generally enriched in groundwater than surface water. We also measured flow velocity using ADCP (Acoustic Doppler Current Profiler). 222Rn concentration in lake water was totally high compared with the offshore water. It suggests the nearshore water is influenced by LGD. Water level changed about 5 cm and observed maximum velocity was ± 0.2~0.3 m3/s during the period. It indicates exchange process between nearshore water and offshore water occurred in the study area. 222Rn concentration tended to decrease with the increase of water exchange.