Related Experiment Video
Updated: Aug 30, 2025

06:28
Field Measurement of Effective Leaf Area Index using Optical Device in Vegetation Canopy
Published on: July 29, 2021
3.4K
Measuring turfgrass canopy interception and throughfall using co-located pluviometers
Don Wesley Dyer1, Andres Patrignani2, Dale Bremer1
1Department of Horticulture and Natural Resources, Kansas State University, Manhattan, Kansas, United States of America.
Plos One
|September 2, 2022
Summary
Turfgrass canopies intercept significant water, with zoysiagrass and creeping bentgrass capturing at least 4.4 mm before any reaches the soil. Small precipitation events are inefficient due to this canopy interception.
Area of Science:
- Horticultural Science
- Environmental Science
- Water Management
Background:
- Turfgrass management frequently involves watering, yet irrigation strategies often overlook canopy interception.
- Canopy interception is the process where water evaporates from plant surfaces before reaching the soil.
Purpose of the Study:
- Quantify precipitation interception and throughfall in 'Meyer' zoysiagrass and '007' creeping bentgrass.
- Evaluate the impact of canopy interception on water reaching the soil surface.
Main Methods:
- Utilized co-located pluviometers with and without turfgrass patches to measure interception and throughfall.
- Collected data from 15 storms and 25 rainfall events, with precipitation ranging from 0.3 mm to 42.4 mm.
Main Results:
- A strong positive linear relationship (r = 0.98) was observed between throughfall amount and precipitation totals.
- Zoysiagrass and creeping bentgrass canopies intercepted an average of 4.4 mm before throughfall.
- Post-throughfall, 16% of additional precipitation/irrigation was lost to interception.
Conclusions:
- No precipitation reaches the soil surface for events under 4.4 mm on average.
- Canopy interception significantly impacts water availability in turfgrass systems, especially in regions like the contiguous U.S.
- Small precipitation and irrigation events are inefficient for turfgrass due to substantial interception losses.
Related Concept Videos
Precipitation Gravimetry
7.0K
Precipitation gravimetry is based on converting an analyte into a sparingly soluble precipitate, which is separated by filtration and weighed. An ideal precipitate should be pure, insoluble, of known composition, and easily filtered from the reaction mixture.
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
In determining nickel by gravimetric analysis, a precipitant of ethanolic dimethylglyoxime is added to a hot nickel salt solution. This is quickly followed by the dropwise addition of dilute ammonia solution until precipitation occurs. A...
7.0K
Precipitation and Co-precipitation
1.9K
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
1.9K
Precipitation Titration: Endpoint Detection Methods
2.0K
In argentometric precipitation titrations, endpoints can be detected visually by the Mohr, Volhard, and Fajans methods. In the Mohr method, adding a soluble chromate indicator gives an initial yellow color to the analyte solution. As the titrant is added, the first excess of silver ions forms a red silver chromate precipitate, marking the endpoint. The solution pH should be maintained at about 8 by adding solid CaCO3.
In the Volhard method, a standard excess of AgNO3 is first added to the...
In the Volhard method, a standard excess of AgNO3 is first added to the...
2.0K
Measurement of Fluid Pressure
284
Fluid pressure is commonly measured using devices called manometers, which rely on liquid columns to indicate pressure differences. The height of a liquid column in a manometer reflects the pressure exerted by the fluid, providing a simple yet effective means of measurement. Different types of manometers serve specific purposes based on their configurations and the type of fluids involved.
A basic form of manometer is the piezometer, a vertical tube open at the top and filled with the same...
A basic form of manometer is the piezometer, a vertical tube open at the top and filled with the same...
284

