Estimation of Actual Evapotranspiration and Crop Coefficient of Transplanted Puddled Rice Using a Modified Non-Weighing Paddy Lysimeter

oleh: Arti Kumari, Ashutosh Upadhyaya, Pawan Jeet, Nadhir Al-Ansari, Jitendra Rajput, Prem K. Sundaram, Kirti Saurabh, Ved Prakash, Anil K. Singh, Rohan K. Raman, Venkatesh Gaddikeri, Alban Kuriqi

Format: Article
Diterbitkan: MDPI AG 2022-11-01

Deskripsi

Lysimetric and eddy covariance techniques are commonly used to directly estimate actual crop evapotranspiration (<inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>E</mi><msub><mi>T</mi><mi>a</mi></msub></mrow></semantics></math></inline-formula>). However, these technologies are costly, laborious, and require skills which make in situ ET estimation difficult, particularly in developing countries. With this in mind, an attempt was made to determine <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>E</mi><msub><mi>T</mi><mi>a</mi></msub></mrow></semantics></math></inline-formula> and stagewise crop coefficient (K<sub>c</sub>) values of transplanted puddled rice using a modified non-weighing paddy lysimeter. The results were compared to indirect methods, viz., FAO Penman–Monteith and pan evaporation. Daily <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>E</mi><msub><mi>T</mi><mi>a</mi></msub></mrow></semantics></math></inline-formula> ranged from 1.9 to 8.2 mmday<sup>−1</sup>, with a mean of 4.02 ± 1.35 mmday<sup>−1</sup>, and their comparison showed that the FAO Penman–Monteith equation performed well for the coefficient of determination (R<sup>2</sup> of 0.63), root mean squared error (RMSE = 0.80), and mean absolute percentage error (MAPE = 13.6 %), and was highly correlated with <inline-formula><math xmlns="http://www.w3.org/1998/Math/MathML" display="inline"><semantics><mrow><mi>E</mi><msub><mi>T</mi><mi>a</mi></msub></mrow></semantics></math></inline-formula> throughout the crop season. However, the pan evaporation approach was underestimated (R<sup>2</sup> of 0.24; RMSE = 0.98; MAPE = 22.13%) due to a consistent pan coefficient value (0.71), vegetation role and measurement errors. In addition, actual K<sub>c</sub> values were obtained as 1.13 ± 0.13, 1.27 ± 0.2, 1.23 ± 0.16, and 0.93 ± 0.18 for the initial, crop development, mid-season, and end-season stages, respectively. These estimated crop coefficient values were higher than FAO K<sub>c</sub> values. Statistical analysis results revealed that the overall stagewise-derived average K<sub>c</sub> values were in line with FAO values, but different from the derived pan K<sub>c</sub> values, although found insignificant at a 5% significance level. In addition, water productivity and agro-meteorological indices were derived to evaluate the cultivar performance in this experiment. Therefore, such a methodology may be used in the absence of weighing lysimeter-derived K<sub>c</sub> values. The derived regional K<sub>c</sub> values can be applied to improve irrigation scheduling under similar agro-climatic conditions.