2022
DOI: 10.1002/agj2.21013
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Response of maize hybrids under limited irrigation capacities: Yield and yield components

Abstract: Grain yield of maize (Zea mays L.) in the semiarid Texas High Plains (THP) is greatly reduced when irrigation cannot meet peak water requirements. Drought‐tolerant hybrids may mitigate yield losses resulting from water deficits. We examined the effect of irrigation capacity (8.47 and 4.23 mm d–1) and planting rates (74,000 and 95,000 seeds ha–1) during three growing seasons (2016–2018) on grain yield and yield components of three maize hybrids, two of which were considered drought tolerant. Crop water deficits… Show more

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“…In addition, these hybrid × irrigation capacity treatment combinations were examined under seeding rates considered to be conservative (74,000 ha −1 ) and high density (95,000 ha −1 ) to evaluate interactions between water stress and plant density. Responses of grain yield, yield components, and water use efficiency to hybrids, imposed irrigation capacities, and plant densities are presented in detail in Schwartz et al (2022).…”
Section: Core Ideasmentioning
confidence: 99%
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“…In addition, these hybrid × irrigation capacity treatment combinations were examined under seeding rates considered to be conservative (74,000 ha −1 ) and high density (95,000 ha −1 ) to evaluate interactions between water stress and plant density. Responses of grain yield, yield components, and water use efficiency to hybrids, imposed irrigation capacities, and plant densities are presented in detail in Schwartz et al (2022).…”
Section: Core Ideasmentioning
confidence: 99%
“…The neutron probe used in this study was previously calibrated in 2002 using methods described by Evett and Steiner (1995) with separate equations for the A, Bt, and Btk horizons. Crop evapotranspiration (ET a ) was estimated based on soil water balance evaluations from planting to harvest maturity, defined as attainment of a grain moisture content of approximately 250 g kg −1 , which occurred 8-18 d after black layer (see Schwartz et al, 2022). Soil water balance was obtained by summing the change in stored soil water (0-1.4 m) based on neutron probe measurements, accumulated precipitation, gross irrigation, runoff, and drainage fluxes using the methods presented by Schwartz et al (2020) to calculate drainage and runoff.…”
Section: Instrumentationmentioning
confidence: 99%
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