More than 35% of the world’s population live within 100 km of the coast. Groundwater resources in these areas are the main source for domestic, industrial and agricultural use. Worldwide, deltaic areas are under stress due to climate change, sea level increase and decrease in fresh water availability. In addition, in deltaic coastal areas around mean sea level, the saline groundwater will move toward the ground surface and exflitrate to surface water. This saline surface water will not be appropriate for drinking water production, agricultural and industrial use, and therefore, freshwater diverted from rivers is used for flushing the canals and ditches in coastal areas. Due to decreasing fresh water availability and increasing surface water...
Rapid discharge of excess water has always been the core of Dutch water management. Due to climate c...
Upward saline groundwater seepage is leading to surface water salinization of deep lying polders in ...
Upward saline groundwater seepage is leading to surface water salinization of deep lying polders in ...
More than 35% of the world’s population live within 100 km of the coast. Groundwater resources in th...
AbstractMore than 35% of the world's population live within 100km of the coast. Groundwater resource...
POLDERS are low-lying and artificially drained areas surrounded bywater storage canals. In low-lying...
Surface water salinization in deltaic areas due to saline groundwater exfiltration is an important i...
Surface water salinization in deltaic areas due to saline groundwater exfiltration is an important i...
Surface water salinization in deltaic areas due to saline groundwater exfiltration is an important i...
Worldwide, delta areas are under stress due to climate change. With rising sealevels and decreasing ...
A significant increase in surface water salinization in low-lying deltas is expected globally due to...
Presence or saline or brackish water in the groundwater system can make lowland areas like polders, ...
Rapid discharge of excess water has always been the core of Dutch water management. Due to climate c...
Upward saline groundwater seepage is leading to surface water salinization of deep lying polders in ...
Upward saline groundwater seepage is leading to surface water salinization of deep lying polders in ...
More than 35% of the world’s population live within 100 km of the coast. Groundwater resources in th...
AbstractMore than 35% of the world's population live within 100km of the coast. Groundwater resource...
POLDERS are low-lying and artificially drained areas surrounded bywater storage canals. In low-lying...
Surface water salinization in deltaic areas due to saline groundwater exfiltration is an important i...
Surface water salinization in deltaic areas due to saline groundwater exfiltration is an important i...
Surface water salinization in deltaic areas due to saline groundwater exfiltration is an important i...
Worldwide, delta areas are under stress due to climate change. With rising sealevels and decreasing ...
A significant increase in surface water salinization in low-lying deltas is expected globally due to...
Presence or saline or brackish water in the groundwater system can make lowland areas like polders, ...
Rapid discharge of excess water has always been the core of Dutch water management. Due to climate c...
Upward saline groundwater seepage is leading to surface water salinization of deep lying polders in ...
Upward saline groundwater seepage is leading to surface water salinization of deep lying polders in ...