How to Make Water Run Uphill

Abstract

A surface having a spacial gradient in its surface free energy was capable of causing drops of water placed on it to move uphill. This motion was the result of an imbalance in the forces due to surface tension acting on the liquid-solid contact line on the two opposite sides ('uphill' or 'downhill') of the drop. The required gradient in surface free energy was generated on the surface of a polished silicon wafer by exposing it to the diffusing front of a vapor of decyltrichlorosilane. The resulting surface displayed a gradient of hydrophobicity (with the contact angle of water changing from 97 deg. to 25 deg.) over a distance of 1 centimeter. When the wafer was tilted from the horizontal plane by 15 deg., with the hydrophobic and lower than the hydrophilic, and a drop of water (1 to 2 microliters) was placed at the hydrophobic end, the drop moved toward the hydrophilic end with an average velocity of about 1 to 2 mm/sec. In order for the drop to move, the hysteresis in contact angle on the surface had to be low (< or = 10 deg.)

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Document Details

Document Type
Technical Report
Publication Date
Jul 01, 1992
Accession Number
ADA254852

Entities

People

  • George M. Whitesides
  • Manoj K Chaudhury

Organizations

  • Harvard University

Tags

Communities of Interest

  • Advanced Electronics
  • Air Platforms
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Chemistry
  • Corporations
  • Energy
  • Free Energy
  • Hydrophilic Properties
  • Hydrophobic Properties
  • Materials
  • Materials Science
  • Measurement
  • Military Research
  • Monomolecular Films
  • Phase
  • Physical Chemistry
  • Surface Tension
  • Thickness
  • Universities
  • Vapor Phases

Readers

  • Atmospheric Science / Meteorology, specifically Wind Wave Turbulence.
  • Mathematics or Statistics
  • Thin Film Deposition Science.