AIMOLI ’s world-leading groundwater flow velocity and direction technology, combined with Professor John A. Cherry’s world-leading stratified detection technology, will definitely take international groundwater research technology to the next level.
Last week, Academician of the Royal Society of Canada and top international expert in groundwater, Academician John A. Cherry, and Professor Jiao Jiujiu of the University of Hong Kong visited Emori for inspection and research.
Professor John A. Cherry is a foreign academician of the National Academy of Engineering (USA), an academician of the Royal Society of Canada, and has received numerous awards and honors from scientific and professional organizations in Canada, the United States, and the United Kingdom. Due to his global contributions to groundwater knowledge and technology, he received the 2016 Lee Kuan Yew Water Prize (Singapore) and the 2020 Stockholm Water Prize.
His research focuses on the cooperativity of groundwater systems and multidisciplinary research. His work involves the chemical evolution of natural and contaminated water in unfractured and fractured aquifers and weak aquifers, as well as the development of engineering groundwater monitoring systems.
At the AIMOLI factory, Professor John A. Cherry visited many of our products, and what surprised him the most was our AIMOLI AML920 groundwater flow velocity and direction instrument.
Why? There are mainly three reasons:
- Professor John A. Cherry’s research mainly focuses on groundwater stratified monitoring technology. Although his research achievements already rank among the top two in the world in this subfield, the data indicators he uses are relatively single. However, underground conditions are relatively complex, and groundwater flow velocity and direction, as well as downhole digital television, can increase the reference dimensions of groundwater stratified monitoring, making groundwater stratified monitoring data more accurate.
- However, traditional groundwater flow velocity and direction detection methods are greatly affected by water pressure, are prone to inaccurate measurements, and peer detection water depth usually only stays within 100 meters, which causes many problems in practical applications. For Professor John A. Cherry’s research direction, this risk is too large; it is better not to use it than to use it.
Our AIMOLI AML920 groundwater flow velocity and direction instrument has a diameter of only 45 mm, low flow velocity ≤1 μm/s, and integrates diversified functions such as display, storage, output, and communication, which peers cannot achieve.
We also adopt the particle tracing method. No matter whether the groundwater is too clear or too turbid, it can be measured accurately, and the water flow can be seen. Even more impressive is that we can reach a maximum depth of 4000 meters, surpassing world first-tier brands.
- In groundwater flow velocity and direction technology, current global peers are still at two-dimensional planar data, while Emori has already adopted a three-dimensional vector algorithm, which is a groundwater condition broadcast. The two are one generation apart. We have 6 standard parameters, and users can optionally add more than 10 hydrological and water quality parameters, which peers truly cannot do.
These performance parameters of the AIMOLI AML920 groundwater flow velocity and direction instrument are of great help to Professor John A. Cherry’s further research on groundwater stratified monitoring technology.
In this investigation, we reached a deep cooperation consensus. AIMOLI ’s world-leading groundwater flow velocity and direction technology, combined with Professor John A. Cherry’s world-leading groundwater stratified monitoring technology, will definitely take international groundwater research technology to the next level.
Professor John A. Cherry highly recognized the innovation of our AIMOLI AML920 groundwater flow velocity and direction instrument, and praised it many times, saying that it is very remarkable that Emori can achieve this level in this niche field.
In fact, the research and development of our AML920 groundwater flow velocity and direction instrument not only involves precision optical imaging, high-definition video processing, particle motion intelligent algorithms and other core optoelectronic technologies, but also can truly restore the original motion state of groundwater, making monitoring data represent real hydrological laws.
Many peers can only achieve “approximate measurement.” The data results are often superficial and far from the real hydrological and geological data, and even contradictory situations occur, lacking practical reference value and scientific persuasiveness.
Here, we sincerely thank Professor John A. Cherry and Professor Jiao Jiujiu for their guidance.
AIMOLI environmental instrument, accurate to the point where competitors are anxious.
