Differences in soil evaporation between row and interrow positions in furrowed agricultural fields

4Citations
Citations of this article
12Readers
Mendeley users who have this article in their library.

Abstract

Although large-scale center pivot sprinkler irrigation has replaced surface irrigation in many locations, the agricultural practice of growing crops in furrows remains common. Still, how the presence of elevated soil rows under sprinkler irrigation influences evaporation losses remains unclear, even while quantifying nonproductive water losses becomes increasingly important for informing new water conservation and irrigation strategies. In this study at the Hermiston Agricultural Research and Extension Center in Hermiston, OR, soil evaporation from the row and interrow positions within potato (Solanum tuberosum L.) fields of contrasting irrigation timing (daytime vs. nighttime) was estimated based on hydrogen and oxygen isotope ratios. Samples collected throughout the 2016 growing season were analyzed and used to calculate soil evaporation (E) losses relative to applied irrigation (I). On average, row positions were more enriched in heavy isotopes than interrow positions, indicating that the evaporated fraction of applied irrigation (E/I) depends on the position. Within the day-irrigated field, the estimated (mean ± standard deviation) E/I ratios determined from both stable isotopes for May, July, and September were 18 ± 8%, 10 ± 3%, and 19 ± 5% for row and 15 ± 6%, 7 ± 2%, and 12 ± 4% for interrow samples. Within the night-irrigated field during these same months, the E/I ratios were 13 ± 12%, 16 ± 7%, and 13 ± 5% for row and 12 ± 7%, 9 ± 2%, and 6 ± 2% for interrow samples, respectively. For these fields, these results reveal that there is more evaporation from row, as compared with interrow, positions. Therefore, management practices for water conservation should account for larger nonproductive evaporation from within rows in order to minimize evaporative losses.

References Powered by Scopus

Liquid-vapor fractionation of oxygen and hydrogen isotopes of water from the freezing to the critical temperature

727Citations
N/AReaders
Get full text

Isotope effects in the evaporation of water: A status report of the Craig-Gordon model

206Citations
N/AReaders
Get full text

High resolution pore water δ<sup>2</sup>H and δ<sup>18</sup>O measurements by H<inf>2</inf>O<inf>(liquid)</inf>-H<inf>2</inf>O <inf>(vapor)</inf> equilibration laser spectroscopy

183Citations
N/AReaders
Get full text

Cited by Powered by Scopus

The NEON Daily Isotopic Composition of Environmental Exchanges Dataset

8Citations
N/AReaders
Get full text

Local-scale evaporation and water loss distribution in surface soil as related to near-surface wind conditions and surface geometry

6Citations
N/AReaders
Get full text

Soil moisture loss and movement between non-grain farmland and typical farmland on the Eastern Loess Plateau: Evidence from stable isotope

0Citations
N/AReaders
Get full text

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Cite

CITATION STYLE

APA

Al-Oqaili, F., Good, S. P., Frost, K., & Higgins, C. W. (2020). Differences in soil evaporation between row and interrow positions in furrowed agricultural fields. Vadose Zone Journal, 19(1). https://doi.org/10.1002/vzj2.20086

Readers over time

‘20‘21‘22‘23‘2401234

Readers' Seniority

Tooltip

Researcher 4

50%

PhD / Post grad / Masters / Doc 2

25%

Professor / Associate Prof. 1

13%

Lecturer / Post doc 1

13%

Readers' Discipline

Tooltip

Environmental Science 2

40%

Agricultural and Biological Sciences 1

20%

Chemistry 1

20%

Engineering 1

20%

Save time finding and organizing research with Mendeley

Sign up for free
0