Ini adalah proses yang sangat sensitif.

Laboratorium Tests for Hydraulic Konduktivity

Kami akan memberikan satu set pada mereka untuk mengatur sistem yang mengatur kondisi yang ada di sana untuk mengurangi aliran hidrolik.

Kalkulations are baseline on Darcy 's law, which relates flow rate, hydralic gradient, and the crostionaI area of the sample. Te formula for hydroulictivity (K) in laboratory tests i:

1f 1f; FLT: 0 133; K = (Q * L) / (A * AFH) S01; FLT: 1: 1; ASA3;

Dimana kita akan melakukan sesuatu, L is the length of the sample, A is the crossing - sectionala area, and voush thoe hydroulic headid diferenco.

Field Tests for Hydraulic Conductivity

Tests field assess hydrolic conductivity idu situ, providing data tont reflects naturaI conditions. Common methog include slug techs, pump tests, and aquifer test. Theste invocate mesuring the change in water over, and afer after a disgubIe.

Ini adalah analysis often uses thees or Cooper - Jacob methog to water lesar data and estimates k. Theese methodes involve plotting drawdown versum time and fitting the data a mathematitical model.

Summary of Calculation Steps

  • Konduct the laboratory or field following standard prosedures.
  • Measure relevant paremeters such as flow rate, head diference, or water level change.
  • Apply Darcy 's law or interpret data using acuate model.
  • Kalkulate hydralic conductivity using the formula or methodas deskripbed.