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Root growth, water potential and yield of irrigated wheat.

Authors :
Mishra, H. S.
Rathore, T. R.
Tomar, V. S.
Source :
Irrigation Science; Jan1999, Vol. 18 Issue 3, p117-123, 7p
Publication Year :
1999

Abstract

Root length density (LV), mid-day leaf water potential ( Ψ<subscript>leaf</subscript>) and yield of wheat were studied in 1983 – 1984 and 1984 – 1985 on a Phoolbagh clay loam (Typic Haplaquoll) and on a Beni silty clay loam (Aquic Hapludoll) in the Tarai region of Uttar Pradesh under naturally fluctuating shallow (0.4 – 0.9 m, SWT) and medium-depth (0.8 – 1.3 m, MWT) water table conditions with six water regimes: rainfed (I<subscript>0</subscript>); irrigation at cown root initiation (I<subscript>1</subscript>); at crown root initiation and milk (I<subscript>2</subscript>); at crown root initiation, maximum tillering and milk (I<subscript>3</subscript>); at crown root initiation, maximum tillering, flowering and milk (I<subscript>4</subscript>); and at crown root initiation, maximum tillering, flowering, milk and dough (I<subscript>5</subscript>). Maximum rooting depth (0.8 m under SWT and 1.05 m under MWT conditions) was attained at the dough stage (115 days after sowing, DAS) and was more strongly influenced by fluctuations in water table depth than by the water regime. For wet regimes (I<subscript>2</subscript>– I<subscript>5</subscript>), roots were concentrated at and above the water table interface and had greater horizontal development, whereas in dry regimens (I<subscript>0</subscript> and I<subscript>1</subscript>), due to deficient moisture conditions in the upper soil layer (0.45 m) they invaded lower horizons and had a greater vertical distribution Ψ<subscript>leaf</subscript> was not significantly affected by water regime (I<subscript>1</subscript>– I<subscript>5</subscript>) up to 94 DAS during a wet year (1983 – 1984) and up to 74 DAS during a dry year (1984 – 1985), but was significantly affected thereafter. Grain yields with water regimens I<subscript>1</subscript>– I<subscript>5</subscript> during a wet year and for the I<subscript>2</subscript>– I<subscript>5</subscript> treatments during a dry year at either water table depth were not significantly different, but there was a (non-significant) trend to lower yield with increasing soil water deficit. Under SWT in I<subscript>2</subscript>, the average grain yield wsa 5130 kg ha<superscript>–1</superscript> and under the I<subscript>3</subscript> regime, 5200 kg ha<superscript>–1</superscript>. Likewise, under MWT in I<subscript>3</subscript>, it was 5188 kg ha<superscript>–1</superscript> and under the I<subscript>4</subscript> regime, 5218 kg ha<superscript>–1</superscript>. The results indicate that application of irrigation of more than 120 and 180 mm under SWT and MWT conditions, respectively, did not raise yield. Irrigation given as per schedule I<subscript>2</subscript> under SWT and I<subscript>3</subscript> under MWT conditions in the Tarai situation, appears to be more effective than a very wet regime (I<subscript>5</subscript>). [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
03427188
Volume :
18
Issue :
3
Database :
Complementary Index
Journal :
Irrigation Science
Publication Type :
Academic Journal
Accession number :
49968973
Full Text :
https://doi.org/10.1007/s002710050052