4.6 Article

Sensitivity analysis of the SWAP (Soil-Water-Atmosphere-Plant) model under different nitrogen applications and root distributions in saline soils

Journal

PEDOSPHERE
Volume 31, Issue 5, Pages 807-821

Publisher

SCIENCE PRESS
DOI: 10.1016/S1002-0160(21)60038-3

Keywords

accumulated transpiration; agro-hydrological model; dry matter; hydraulic parameter; sunflower; yield

Categories

Funding

  1. Major Program of the National Natural Science Foundation of China [51879196, 51790533]
  2. China Postdoctoral Science Foundation [2020M682475]
  3. Fundamental Research Funds for the Central Universities, China [IWHR-SKL-KF201814]

Ask authors/readers for more resources

This study conducted a variance-based global sensitivity analysis to investigate the impacts of different parameters in an agro-hydrological model on simulated transpiration, dry matter, and yield of sunflowers. Results showed that soil hydraulic parameters, critical stress index for compensatory root water uptake, and salt stress levels had significant impacts on the model outputs under various conditions.
Sensitivity analysis is important for determining the parameters in the model calibration process. In our study, a variance-based global sensitivity analysis (extended Fourier amplitude sensitivity test, EFAST) was applied to an agro-hydrological model (the SWAP (Soil-Water-Atmosphere-Plant model) model). The sensitivities of 20 parameters belonging to 4 categories (soil hydraulics, solute transport, root water uptake, and environmental stresses) for the simulated accumulated transpiration, dry matter (DM), and yield of sunflowers were analyzed under three nitrogen application rates (N1, N2, and N3), four salinity levels (S1, S2, S3, and S4), and three root distributions (R1, R2, and R3). The results indicated that for predominantly loamy soils, the high-impact parameters for accumulated transpiration, DM, and yield were the soil hydraulic parameters (alpha and n), critical stress index for compensatory root water uptake (omega(c)), the salt level at which salt stress starts (Pi), the decline of root water uptake above Pi (SSF), residual water content (theta(r)), saturated water content (theta(s)), and relative uptake of solutes by roots (TSCF). We also found that nitrogen application did not change the order of the parameter impacts on accumulated transpiration, DM, and yield. However, TSCF replaced ff as the highest-impact parameter for the accumulated transpiration, DM, and yield at high salinity levels (S2 and S3). Furthermore, alpha was also the highest-impact parameter for DM and yield under different root distributions, but the highest-impact parameters for transpiration were omega(c), alpha, and theta(s) under R1, R2, and R3, respectively. Nitrogen application could be neglected when considering the interactive effects of nitrogen application, salinity level, and root distribution on the transpiration, DM, and yield. Additionally, the mean values and uncertainties of the transpiration, DM, and yield were similar in all scenarios, except S3, which showed a sharp decrease in the mean values. We suggest determining the above eight parameters (alpha, n, omega(c), Pi, SSF, theta(r), theta(s), and TSCF) and the saturated vertical hydraulic conductivity (K-s) based on rigorous calibrations with direct or indirect local measurements using economical methods (e.g., a literature review), with limited observations for other parameters when using the SWAP model and other similar agro-hydrological models.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.6
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available