2021
DOI: 10.1029/2021wr030747
|View full text |Cite
|
Sign up to set email alerts
|

Estimation of Evapotranspiration Rates and Root Water Uptake Profiles From Soil Moisture Sensor Array Data

Abstract: Evapotranspiration (ET), an amalgam of evaporation from the soil to the atmosphere and plant transpiration in the root zone, is a critical component of the hydrologic cycle. The ability to quantify ET is crucial to science-based predictions of an ecosystem's dynamics and health (Fath, 2018;Fisher et al., 2011); and the impact of droughts, precipitation patterns and snow-melt on groundwater recharge (

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1
1

Citation Types

0
12
0

Year Published

2022
2022
2023
2023

Publication Types

Select...
4

Relationship

1
3

Authors

Journals

citations
Cited by 4 publications
(12 citation statements)
references
References 48 publications
0
12
0
Order By: Relevance
“…Furthermore, since the internal permeability of the swollen SAP is much smaller than the permeability of the soil matrix [49] we treat the SAP as being completely impermeable to water flow. Then, computing the probability that a given point within the SAP-soil mixture is encompassed by a randomly-placed swollen SAP grain [50] yields the new porosity of the SAP-soil mixture, ε = ε control e −ϕ (7) where ϕ = V SAP /V is the total volume fraction occupied by swollen SAP with V SAP = N SAP ν SAP and V ≈ N soil ν soil /(1 − ε control ) representing the total swollen SAP volume (neglecting the soil grains) and the total system volume, respectively. Finally, assuming for simplicity that the hydraulic radius R is set by the soil grain size and is therefore unchanged upon SAP addition, and that the pore space tortuosity is also unchanged upon SAP addition, then yields our final approximate prediction for the SAP-soil mixture permeability k:…”
Section: Results Of Coefficient Of Permeability Measurementsmentioning
confidence: 99%
See 1 more Smart Citation
“…Furthermore, since the internal permeability of the swollen SAP is much smaller than the permeability of the soil matrix [49] we treat the SAP as being completely impermeable to water flow. Then, computing the probability that a given point within the SAP-soil mixture is encompassed by a randomly-placed swollen SAP grain [50] yields the new porosity of the SAP-soil mixture, ε = ε control e −ϕ (7) where ϕ = V SAP /V is the total volume fraction occupied by swollen SAP with V SAP = N SAP ν SAP and V ≈ N soil ν soil /(1 − ε control ) representing the total swollen SAP volume (neglecting the soil grains) and the total system volume, respectively. Finally, assuming for simplicity that the hydraulic radius R is set by the soil grain size and is therefore unchanged upon SAP addition, and that the pore space tortuosity is also unchanged upon SAP addition, then yields our final approximate prediction for the SAP-soil mixture permeability k:…”
Section: Results Of Coefficient Of Permeability Measurementsmentioning
confidence: 99%
“…Optimum management of this resource is particularly important from the point of view of agricultural production or biotechnological solutions used in environmental engineering [4,5]. The physicochemical properties of the upper soil layer will determine the mutual interactions between water infiltration, runoff, and evaporation under given climatic conditions, and therefore influence its usability for supporting plant growth [6,7]. Hence, in recent decades, grains of super-absorbent polymers (SAP) have attracted increasing interest as soil additives to rationally tune these properties and to stabilize the soil [8][9][10].…”
Section: Introductionmentioning
confidence: 99%
“…Algorithm 1 summarizes the EnKF strategy described above. General considerations allow one to expect this algorithm to significantly outperform the previous versions of EnKF used to estimate ET from soil‐moisture data (Li et al., 2021; Pan & Wood, 2006; Reichle et al., 2008) in terms of either accuracy or efficiency or both. Unlike these one‐dimensional methods, Algorithm 1 accounts for the horizontal component of the water flux, which is likely to be pronounced in heterogeneous soils subjected to drip irrigation.…”
Section: Alternative Strategies For Et Estimationmentioning
confidence: 99%
“…A key advantage of ensemble-based (Bayesian) data assimilation (DA) methodologies is that their estimates of the relevant system parameters and state variables are equipped with uncertainty (error) bounds (Boso & Tartakovsky, 2022). Among these tools, ensemble Kalman filter (EnKF) has gained popularity because of computational expediency; among other hydrologic applications, it was used to estimate, from soil-moisture sensor-array data, water content and total ET rate (Pan & Wood, 2006;Reichle et al, 2008) and spatial distributions of ET rates and root water-uptake (Li et al, 2021) in vertical (1D) soil columns.The vertical-flow assumption alleviates the computational cost of ensemble-based DA techniques, for example, variational DA, EnKF and particle filters, and is arguably adequate at the basin scale. At the field scale of interest to smart agriculture, the 1D assumption implies a homogeneous soil with sprinkler/spray irrigation patterns that are similar to rainfall.…”
mentioning
confidence: 99%
See 1 more Smart Citation