1970•Water Resources ResearchRequires access

Evapotranspiration from bare, herbaceous, and aspen plots: A check on a former study

Robert S. Johnston

Open publisher page 28 citations

Abstract

Soil moisture depletion was measured and evapotranspiration estimated on high elevation plots with three cover conditions: bare, herbaceous, and aspen‐herbaceous. Neutron moisture measurements were taken to a depth of 9 feet. The 4‐year average annual evapotranspiration losses were 11.28, 15.27, and 21.00 inches from the bare, herbaceous, and aspen‐herbaceous plots, respectively. Summer rainfall varied from 1.13 to 10.43 inches during this study. Soil moisture depletion to a depth of 6 feet and estimated evapotranspiration on these plots were reported by Croft and Monninger [1953]. The results of this present study substantiate the earlier report concerning the comparative water savings to be realized by vegetative manipulation. They show that removing deep rooted aspen can reduce the average evapotranspiration by about 6 inches per year from a 9‐foot profile.

About this research paper

What this paper is about

Soil moisture depletion was measured and evapotranspiration estimated on high elevation plots with three cover conditions: bare, herbaceous, and aspen‐herbaceous. Neutron moisture measurements were taken to a depth of 9 feet. The 4‐year average annual evapotranspiration losses were 11.28, 15.27, and 21.00 inches from the bare, herbaceous, and aspen‐herbaceous plots, respectively. Summer rainfall varied from 1.13 to 10.43 inches during this study. Soil moisture depletion to a depth of 6 feet and estimated evapotranspiration on these plots were reported by Croft and Monninger [1953]. The results of this present study substantiate the earlier report concerning the comparative water savings to be realized by vegetative manipulation. They show that removing deep rooted aspen can reduce the average evapotranspiration by about 6 inches per year from a 9‐foot profile.

Why it matters

OpenAlex reports 28 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

Soil moisture depletion was measured and evapotranspiration estimated on high elevation plots with three cover conditions: bare, herbaceous, and aspen‐herbaceous. Neutron moisture measurements were taken to a depth of 9 feet. The 4‐year average annual evapotranspiration losses were 11.28, 15.27, and 21.00 inches from the bare, herbaceous, and aspen‐herbaceous plots, respectively. Summer rainfall varied from 1.13 to 10.43 inches during this study. Soil moisture depletion to a depth of 6 feet and estimated evapotranspiration on these plots were reported by Croft and Monninger [1953]. The results of this present study substantiate the earlier report concerning the comparative water savings to be realized by vegetative manipulation. They show that removing deep rooted aspen can reduce the average evapotranspiration by about 6 inches per year from a 9‐foot profile.

Key concepts: Evapotranspiration, Herbaceous plant, Environmental science, Water content, Hydrology (agriculture), Neutron probe, Moisture, Soil water

Related papers

Back to paper searchBrowse research topicsOriginal source
Evapotranspiration from bare, herbaceous, and aspen plots: A check on a former study — Research Paper | ScholarLens