City of Hilla suffers from the shal

City of Hilla suffers from the shallow groundwater levels which causes serious problems to agricultural and civil work activities in the area. To examine these problems, five different tracks perpendicular to the Shatt Al-Hilla channel were selected beside 18 hand dug wells within the area to monitoring the inter-relationships between the levels of both water resources over one complete water year (2011-2012). Field work included monitoring of water levels within the selected wells in the examined area and compares the results with the water levels in the Shatt Al-Hilla over observation period. Elevations of water levelswere determined by comparing to the sea water levels depending upon the bench mark in the examined area. Along each of the selected five tracks ( A, B, C, D and E)three shallow groundwater hand dug wells are monitored exceptalong track D were sixshallow groundwater hand dug wells were monitored. Depthof thesewellsrangesfrom 7 to12 m. The distances of the monitoredwells from Shatt Al-Hilla were ranging from 100m to about and the 1150 m. Thedistancesbetween wellswere ranging from50m to 300m approximately. However, Track (A) and (B) located within the City of Hilla representing shallow groundwater within the residential area while the remaining tracks presenting shallow groundwater situations within nearby agricultural lands.Water levels of both surface and groundwater levels monitored on monthly bases especially over high and low water conditions within Shatt Al-Hilla channel. Dora regulator is located at 51 Km from up stream of Shatt Al-Hilla; it is controlled totally on water levels within Shatt Al-Hilla channel, accordingly Dora regulator will influencing water levels ofthe shallow groundwater.The data shows that there isa strong inter-relationship between surface and shallow groundwater in the studied area. The nature of theseinter-relationship werevarying along the selectedtracks due to many local conditionssuch as, elevations of lands, operation of irrigational regulators, depth of water within the channelcross section,seasons of the water year, high and low water level conditions, climatic changes, soil conditions and the present status of the sewage systemwithin the City of Hilla

النتائج (الإنجليزية) 1:

City of Hilla suffers from the shallow groundwater levels which causes serious problems to agricultural and civil work activities in the area. To examine these problems, five different tracks perpendicular to the Shatt Al-Hilla channel were selected beside 18 hand dug wells within the area to monitoring the inter-relationships between the levels of both water resources over one complete water year (2011-2012). Field work included monitoring of water levels within the selected wells in the examined area and compares the results with the water levels in the Shatt Al-Hilla over observation period. Elevations of water levelswere determined by comparing to the sea water levels depending upon the bench mark in the examined area. Along each of the selected five tracks (A, B, C, D and E) three shallow groundwater hand dug wells are monitored exceptalong track D were sixshallow groundwater hand dug wells were monitored. Depthof thesewellsrangesfrom 7 to12 m. The distances of the monitoredwells from Shatt Al-Hilla were ranging from 100m to about and the 1150 m. Thedistancesbetween wellswere ranging from50m to 300m approximately. However, Track (A) and (B) located within the City of Hilla representing shallow groundwater within the residential area while the remaining tracks presenting shallow groundwater situations within nearby agricultural lands.Water levels of both surface and groundwater levels monitored on monthly bases especially over high and low water conditions within Shatt Al-Hilla channel. Dora regulator is located at 51 Km from up stream of Shatt Al-Hilla; it is controlled totally on water levels within Shatt Al-Hilla channel, accordingly Dora regulator will influencing water levels ofthe shallow groundwater.The data shows that there isa strong inter-relationship between surface and shallow groundwater in the studied area. The nature of theseinter-relationship werevarying along the selectedtracks due to many local conditionssuch as, elevations of lands, operation of irrigational regulators, depth of water within the channelcross section, seasons of the water year, high and low water level conditions, climatic changes, soil conditions and the present status of the sewage systemwithin the City of Hilla The data shows that there isa strong inter-relationship between surface and shallow groundwater in the studied area. The nature of theseinter-relationship werevarying along the selectedtracks due to many local conditionssuch as, elevations of lands, operation of irrigational regulators, depth of water within the channelcross section, seasons of the water year, high and low water level conditions, climatic changes, soil conditions and the present status of the sewage systemwithin the City of Hilla The data shows that there isa strong inter-relationship between surface and shallow groundwater in the studied area. The nature of theseinter-relationship werevarying along the selectedtracks due to many local conditionssuch as, elevations of lands, operation of irrigational regulators, depth of water within the channelcross section, seasons of the water year, high and low water level conditions, climatic changes, soil conditions and the present status of the sewage systemwithin the City of Hilla

النتائج (الإنجليزية) 2:

City of Hilla suffers from the shallow groundwater levels which causes serious problems to agricultural and civil work activities in the area. To examine these problems, five different tracks perpendicular to the Shatt Al-Hilla channel were selected beside 18 hand dug wells within the area to monitoring the inter-relationships between the levels of both water resources over one complete water year ( 2011-2012). Field work included monitoring of water levels within the selected wells in the examined area and compares the results with the water levels in the Shatt Al-Hilla over observation period. Elevations of waterwere determined by comparing to the sea water depending upon the bench mark in the examined area. Along each of the selected five tracks (A, B, C, D and E)three shallow groundwater hand dug wells are monitored except track D were six groundshallowwater hand dug wells were monitored. Depthof thesewellsrangesfrom 7 to12 m. The distances of the monitoredwells from Shatt Al-Hilla were ranging from 100m to about and the 1150 m. Thedistancesbetween wellswere ranging from 50m to 300m approximately. However, Track (A) and (B) located within the City of Hilla representing shallow groundwater within the residential area while the remaining tracks presenting shallow groundwater situation within nearby agricultural lands. Water levels of both surface and groundwater levels monitored on monthly bases especially over high and low water conditions within Shatt Al-Hilla channel. Dora regulator is located at 51 Km from up stream of Shatt Al-Hilla; It is totally controlled on water levels within Shatt Al-Hilla channel, accordingly Dora regulator will influencing water levels of the shallow groundwater. The data shows that there is a strong inter-relationship between surface and shallow groundwater in the studied area. The nature of these inter-relationship wasvarying along the selectedtracks due to many local conditions such as, elevations of lands, operation of irrigational regulators, depth of water within the channelcross section, seasons of the water year, high and low water level conditions, climatic changes, soil conditions and the present status of the sewage systemwithin the City of Hilla

النتائج (الإنجليزية) 3:

The shallow groundwater in mountainous cities causes serious problems to the agricultural and recreational activities in this area. Based on the investigation of five different waterways along the Chartres River, 18 hand dug well was selected to monitor the relationship between the water resources above 2011 in this area. The on-site monitoring of the well water level in the mining area includes the monitoring of the well water level in the mining area and the comparison between the monitoring results and the observation period. This standard is applicable to the relationship between the sea water level specified in this standard and the water level in the inspection area. Five tracks, B, C, D and E, are selected for shallow groundwater monitoring The distance from the seventh floor to the M floor ranges from 100m to 1150M from Shatt al Hilla and from 50m to 300m. Hove The representative shallow groundwater in mountainous cities and residential areas maintain the adjacent shallow groundwater conditions, especially the high groundwater level and low groundwater level. Shatt al Hilla channel According to the function of the pressure regulator and the influence of the pressure regulator on the water level of the shallow groundwater, the water level of the shallow groundwater is controlled comprehensively, and the relationship between the shallow groundwater and the shallow groundwater is studied. Local conditions, elevation, water depth of channel section, high water level in the year, microclimate in the year, microclimate in the year, microclimate in the year, microclimate in the year, microclimate in the year Soil conditions and present situation of drainage system in hilly cities