English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

In Lake Kasumigaura where paleohydrologic information during the period of sedimentation may have remained, two-dimensional unsteady groundwater flow simulation was made in vertical cross section while considering such long-term transitions as sea level change, changes in salinity and sedimentation. As a result, the depth profiles of salinity in pore water extracted at two core drilling sites that were obtained in existing works were reproduced, the difference in contribution of local fresh groundwater at both sites was indicated. The simulation revealed that Site K-1, which is close to the lakefront, was affected by local fresh groundwater as well as surface water, but Site K-2, some way distant from the lakefront, was unaffected by the local fresh groundwater. By unsteady groundwater flow simulation, the transition of the more detailed hydrological environment was revealed.

非定常地下水流動解析による霞ヶ浦の完新世における古水文環境の復元