Shoot and root dry weight and soil water in wheat, triticale and rye

1991 ◽  
Vol 71 (1) ◽  
pp. 41-49 ◽  
Author(s):  
Q. Sheng ◽  
L. A. Hunt

Dry matter distribution between the shoots and root was evaluated for three cereal cultivars, one each of wheat (Triticum aestivum L.), triticale (× Triticosecale Wittmack) and rye (Secale cereale L.). Evaluations were made both indoors and outdoors (the Elora Research Station, 43°39′N 80°25′W) at four growth stages. Volumetric soil water content beneath the three species was also measured in the field. There were significant differences (P < 0.01) among the three species in total plant dry weight indoors and outdoors. Although rye consistently had the greatest total plant dry mass, total root dry weight was not greater than for the other species in many comparisons, especially before anthesis. However, rye root growth surpassed all the others after anthesis, and root dry weight was greater at final harvest. Triticale and rye had greater shoot: root ratios than wheat at the later growth stages. Although there were no consistent differences among species in root dry weight distribution at different soil depths, rye had a relatively larger proportion of root dry weight in the upper soil layer than the other species. Species effects on soil water content were significant (P < 0.05) at depths of 15–45 cm and 45–90 cm during a drought period. Water content in the 45–90 cm layer was lower for the triticale cultivar than for the wheat and rye. Key words: Wheat, triticale, rye, shoot:root ratio, volumetric soil water content

2018 ◽  
Vol 10 (6) ◽  
pp. 97-105 ◽  
Author(s):  
Morgan Amanda ◽  
Joseph Pearson Brian ◽  
Shad Ali Gul ◽  
Moore Kimberly ◽  
Osborne Lance

HortScience ◽  
2008 ◽  
Vol 43 (3) ◽  
pp. 952-954 ◽  
Author(s):  
Jorge A. Zegbe ◽  
M. Hossein Behboudian ◽  
Brent E. Clothier ◽  
Alexander Lang

Quality and storability of ‘Pacific Rose™’ apple grown under partial rootzone drying (PRD) were studied over 2 years. The treatments were commercial irrigation (CI) and PRD, which were applied by watering one side of the tree row throughout the season (Expt. 1) or by alternating irrigation between two sides of the tree row when volumetric soil water content ranged between 0.18 and 0.22 m3·m−3 (Expt. 2). The PRD and CI fruit had similar quality attributes at harvest and after storage except that the former had lower weight loss during storage in Exp. 1 and a lower firmness after storage in Exp. 2. Compared with CI, PRD saved water by 0.15 mega liters per hectare in Exp. 1 and by 0.14 mega liters per hectare in Exp. 2. We recommend PRD for humid environments similar to ours.


2004 ◽  
Vol 84 (3) ◽  
pp. 333-338 ◽  
Author(s):  
P. R. Bullock ◽  
X. Li ◽  
L. Leonardi

Critical soil water levels for soil microscale processes are difficult to determine because of variability in large soil volumes and lack of techniques for logging soil water contents in small soil volumes. This study tested nearinfrared (NIR) spectroscopy for soil water content determination. Five soil horizons with a range in soil texture, soil organic carbon, carbonates, pH and horizon depth, were tested at air-dry, field capacity and 0.1 MPa tension water content. Volumetric soil water content, determined using the standard method of oven-drying and soil bulk density, was compared to NIR absorbance in various combinations and wavelengths. The NIR spectra obtained with the probe in direct contact with the soil gave better results than when the probe was separated from the soil with a glass slide. The most reliable validation results were obtained using a multivariate partial least squares regression of the full spectrum with an r2 of 0.95 and RMSE of prediction of 6.4%. Smoothing and derivatives of the spectra did not improve the validation results. The relationships for absorbance at single wavelength segments, ratios, differences and area under the curve around the 1940 nm peak were good (r2 values near 0.85 ) but poorer than the results using the full spectra. The high correlation coefficients obtained with the wide variety of soils utilized in this study suggest that NIR absorbance is a practical method for determining volumetric soil water content for small soil volumes. Key words: Near-infrared spectroscopy, soil water, Near-infrared absorbance


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