{"id":197,"date":"2026-06-27T21:33:12","date_gmt":"2026-06-27T13:33:12","guid":{"rendered":"https:\/\/www.aimoli2016.cn\/?p=197"},"modified":"2026-06-27T21:33:13","modified_gmt":"2026-06-27T13:33:13","slug":"we-have-solved-the-problems-encountered-in-traditional-methods-of-measuring-groundwater-flow-velocity-and-direction","status":"publish","type":"post","link":"https:\/\/www.aimoli2016.cn\/?p=197","title":{"rendered":"We have solved the problems encountered in traditional methods of measuring groundwater flow velocity and direction!"},"content":{"rendered":"\n

Traditional methods for measuring groundwater flow velocity<\/a> and direction in groundwater monitoring<\/a> often encounter three challenges: efficiency and accuracy issues!<\/strong><\/p>\n\n\n\n

1\u3001Long measurement cycle and delayed response: Traditional tracer methods require multi-point sampling and long-term tracking to calculate water flow parameters, and a single complete measurement can take several days or even longer, which cannot meet the rapid response requirements of sudden pollution events.<\/p>\n\n\n\n

2\u3001Large data deviation and weak anti-interference ability: Formation heterogeneity, wellbore adsorption effect, and human operation errors can easily lead to data distortion, especially in low-permeability formations or complex well conditions. Traditional methods often fail due to signal attenuation or interference.<\/p>\n\n\n\n

3\u3001Secondary pollution risk: The addition of chemical tracers may introduce external pollutants, which goes against the original intention of groundwater protection.<\/p>\n\n\n\n

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AIMOLI’s AML920 groundwater flow meter<\/a> technology breakthrough solves the above three problems.<\/strong><\/p>\n\n\n\n

    \n
  1. Non interfering in-situ measurement, reliable data: using particle image recognition technology, abandoning traditional chemical tracing methods, directly obtaining flow velocity and direction data through wellbore imaging and flow field analysis, achieving zero pollution and zero interference in-situ monitoring. Flow velocity accuracy: 0.01 \u03bc m\/s (10 times higher than traditional methods);<\/strong> Flow direction error: within \u00b1 1 \u00b0.<\/li>\n\n\n\n
  2. Multi parameter synchronous acquisition: key indicators such as water temperature, water level, and conductivity are synchronously recorded to provide multidimensional data support for pollution diffusion simulation.<\/li>\n\n\n\n
  3. Full scene adaptation capability, breaking through complex geological limitations: equipped with 360 \u00b0 panoramic and top-down imaging systems,<\/strong> automatically identifying wellbore diameter and accurately positioning, single point measurement only takes 1 hour, and efficiency is improved by more than 5 times; The lightweight design (weight<5kg) and IP68 level protection of the equipment support the rapid deployment and recovery of a single person, and adapt to the harsh environment such as rainstorm, humidity and mud; <\/strong>It can accurately identify hidden channels such as inclined shafts and rock fractures, providing key evidence for locking the path of pollution infiltration.<\/li>\n\n\n\n
  4. Traceability of data and scientific decision-making: Automatically generate three-dimensional flow field vector maps and radar maps, visually presenting the trajectory of groundwater movement; <\/strong>Combining GIS platform to achieve dynamic simulation and traceability analysis of pollution diffusion paths, helping to formulate precise governance plans.<\/li>\n<\/ol>\n\n\n\n

    Why choose AML920 flow meter<\/a>? \u2014\u2014The preferred partner for safeguarding groundwater safety<\/strong><\/p>\n\n\n\n

    Against the backdrop of increasingly strict environmental regulations, the AML920 flow meter has become an ideal tool for chemical parks, environmental monitoring agencies, and geological survey units. It is widely used in pollution tracing, aquifer assessment, ecological restoration, and other scenarios, providing protection for groundwater safety.<\/p>\n\n\n\n

    \"\"<\/figure>\n","protected":false},"excerpt":{"rendered":"

    Traditional methods for measuring groundwater flow velocity and direction in groundwater monitoring often encounter three challenges: efficiency and accuracy issues! 1\u3001Long measurement cycle and delayed response: Traditional tracer methods require multi-point sampling and long-term tracking to calculate water flow parameters, and a single complete measurement can take several days or even longer, which cannot meet […]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-197","post","type-post","status-publish","format-standard","hentry","category-blog"],"aioseo_notices":[],"aioseo_head":"\n\t\t\n\t\n\t\n\t\n\t\n\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t