{"id":9356,"date":"2020-08-05T14:48:12","date_gmt":"2020-08-05T09:48:12","guid":{"rendered":"http:\/\/cewre.edu.pk\/web\/?page_id=9356"},"modified":"2025-09-25T20:49:00","modified_gmt":"2025-09-25T15:49:00","slug":"hydrology-lab","status":"publish","type":"page","link":"https:\/\/cewre.edu.pk\/web\/hydrology-lab\/","title":{"rendered":"Hydrology Lab"},"content":{"rendered":"

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This laboratory is equipped with TV. Bore Hole Camera, Current Meters, Survey and Leveling Instruments, Depth Recorders, Water Level Recorders, Earth Resistivity Meters, and instruments for evaporation studies. This laboratory provides facilities for resistivity surveys, hydrometeorology studies, detecting faults in tubewell bore holes, measuring discharge of the distributaries and canals, measurements of the depth of rivers and lakes.<\/p>\n

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Water Level Statistics at UET Lahore (2019-24)<\/h3>\n

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Lahore-capital of Punjab Province is totally dependent on groundwater reserves for its domestic and industrial uses. High abstraction rates in Lahore has declined its water table and is continuously declining. Lahore Development Authority (LDA) in collaboration with UET Lahore had installed four recharging wells of large diameter in Junaid Jamshed Cricket Stadium of UET, Lahore. Piezometer having 150 feet depth and 2-inch diameter is installed to monitor groundwater behavior. Also, a recharging well is installed at Anexy Ground. The graphs given below shows the temporal change in water level from mean average sea level (in meters) during 2019-24 at UET, Lahore.<\/p>\n

[\/vc_column_text][vc_single_image image=”13751″ img_size=”full” alignment=”center” css_animation=”appear”][vc_single_image image=”14172″ img_size=”full” alignment=”center” css_animation=”appear”][\/vc_column_inner][\/vc_row_inner][vc_tta_accordion style=”modern” color=”green” c_icon=”chevron” c_position=”right” active_section=”” no_fill=”true” collapsible_all=”true” css=”.vc_custom_1610437355232{margin-top: 5% !important;margin-bottom: 5% !important;}”][vc_tta_section title=”LIST OF EXPERIMENTS AT LAB” tab_id=”1610430118950-924d43cb-b221″][vc_column_text]<\/p>\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n\n
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Exp. No.<\/strong><\/h6>\n<\/th>\n
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Experiment Title<\/strong><\/h6>\n<\/th>\n
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Apparatus<\/strong><\/h6>\n<\/th>\n
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Read<\/strong><\/h6>\n<\/th>\n
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Download<\/strong><\/h6>\n<\/th>\n<\/tr>\n
1.<\/td>\n1<\/td>\nTo Understand Storm Hydrograph<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
2.<\/td>\n2<\/td>\nTo generate overland flow<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
3.<\/td>\n3<\/td>\nTo understand the initiation and characteristics of bedload motion<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
4.<\/td>\n4<\/td>\nTo understand the effect of changing stream power and channel morphology<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
5.<\/td>\n5<\/td>\nTo understand the effect of base level change<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
6.<\/td>\n6<\/td>\nTo understand the scour in open channel flow<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
7.<\/td>\n7<\/td>\nTo study the water abstraction from a well in a confined aquifer<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
8.<\/td>\n8<\/td>\nTo study the water abstraction from a well in an unconfined aquifer<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
9.<\/td>\n9<\/td>\nTo study the water abstraction from a number of neighbouring wells<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
10.<\/td>\n10<\/td>\nTo study the effect of rainfall on a circular island with a central well<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
11.<\/td>\n11<\/td>\nTo study the ground water flow between two canals with and without rainfall<\/td>\nAdvanced Hydrological Apparatus<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
12.<\/td>\n–<\/td>\nAuto Level Experiments<\/td>\nAuto Level with Accessories<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
13.<\/td>\n–<\/td>\nTheodolite Experiments<\/td>\nTheodolite with Accessories<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n
14.<\/td>\n–<\/td>\nWater Level Indicator<\/td>\n—<\/td>\n
Read More<\/strong><\/a><\/center><\/td>\n
Download<\/strong><\/a><\/center><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n

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