Improved understanding of soil water content at field capacity and estimates from pedotransfer functions

Author:

Andabili Samira Jaefarzade1ORCID,Rasoulzadeh Ali1ORCID,Moghadam Javad Ramezani1ORCID,Pollacco Joseph Alexander Paul2ORCID,Fernández‐Gálvez Jesús3ORCID

Affiliation:

1. Water Engineering Department, Faculty of Agriculture and Natural Resources University of Mohaghegh Ardabili Ardabil Iran

2. Manaaki Whenua – Landcare Research Lincoln New Zealand

3. Department of Regional Geographic Analysis and Physical Geography University of Granada Spain

Abstract

AbstractThe soil water content at field capacity, θFC, is a fundamental variable for irrigation and agriculture. This study determines the optimal tension (−33 or −10 kPa) of deriving θFC which best matches the in situ field measurements following the Veihmeyer procedure. The Veihmeyer method refers to a profile water status for which there is a negligible drainage rate of bare soil without evaporation. In addition, we derive a set of linear and nonlinear pedotransfer functions (PTFs) which estimate θFC. θFC was measured in 69 plots in north‐western Iran, which has a cold semi‐arid climate. The soil properties used for developing PTFs include texture, bulk density, and organic matter. The results show that θFC cannot be derived at a fixed tension. We therefore developed PTFs with satisfactory performance in reproducing in situ measured θFC. The findings show that PTFs developed at a fixed tension consistently underestimate θFC derived in situ. It was also speculated that tension less than −10 kPa could yield improved predictions of in situ θFC.

Funder

University of Mohaghegh Ardabili

Publisher

Wiley

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