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Vergara - 1976 - Physiological and morphological adaptability of ri

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249<br />

Temperature <strong>and</strong> the chemical<br />

kinetics <strong>of</strong> flooded soils<br />

F. Ponnamperuma<br />

SUMMARY<br />

oil temperature is an impoitant factor determining the growth <strong>and</strong> yield <strong>of</strong><br />

<strong>ri</strong>ce in submerged soils. Apart from its direct influence on the physiology<br />

<strong>of</strong> the roots <strong>and</strong> other submerged part. <strong>of</strong> the plants. soil temperature markedly<br />

affects the nut<strong>ri</strong>tion <strong>of</strong> the <strong>ri</strong>ce plant through its effects on the chemical kinetics<br />

<strong>of</strong> the soil.<br />

Laboratory" <strong>and</strong> greenhouse studies on the chemical kinetics <strong>of</strong>a total <strong>of</strong> 20<br />

submerged soils maintained at l5‘. 25*‘. 35"’. <strong>and</strong> 45C or 38° ' 20C. 30°C. 15°<br />

'<br />

"<br />

31° llPC. <strong>and</strong> 20°C revealed that the 35° <strong>and</strong> 33° " 20°C regimes produced<br />

a rapid increase in pII <strong>of</strong> acid stiils. rapid <strong>and</strong> narrow‘ peaks <strong>of</strong> carbon<br />

dioxide. volatile organic acids. reducing substances. <strong>and</strong> ferrous iron; <strong>and</strong> an<br />

increased supply <strong>of</strong> anunonia <strong>and</strong> phosphate, compared with the other temperature<br />

regimes. Temperatures below 25°C brought about a slow build-up <strong>of</strong> high<br />

<strong>and</strong> persistent concentrations <strong>of</strong> carbon dioxide. volatile organic acids. ferrous<br />

iron, <strong>and</strong> reducing substances, especially i11 the acid soils. A constant temperature<br />

<strong>of</strong> 45°C leads to the production <strong>of</strong> high concentrations <strong>of</strong> reducing substances<br />

<strong>and</strong> carbon dioxide.<br />

INTRODUCTION<br />

Growth <strong>and</strong> yield <strong>of</strong> <strong>ri</strong>ce was best under the 35°C <strong>and</strong> 38° " 20°C regimes,<br />

<strong>and</strong> poorest below 20°C <strong>and</strong> at 45°C. The adverse effects <strong>of</strong> low temperature<br />

were more scvcrc 011 acid soils than 011 neutral soils.<br />

The temperature regimes in flooded <strong>ri</strong>ce soils vary wldClfy’. In the temperate<br />

zone, soil temperature may range from 15°C at planting to 40°C in late summer.<br />

In the subtropics, for the second crop, soil temperature declines as the crop<br />

matures. The two main temperature regimes. in the tropics are fairly constant<br />

temperatures <strong>of</strong> about 30°C at sea level <strong>and</strong> about 20°C in the highl<strong>and</strong>s.<br />

Rice physiologists have studied extensively‘ the effects <strong>of</strong> temperature on germination.<br />

growth. flowe<strong>ri</strong>ng, grain fo1mation_ <strong>and</strong> the uptake <strong>of</strong> nut<strong>ri</strong>ents.<br />

chiefly from culture solutions (Matsuda, 1930; Takahashi ct al.. 1955; Sasaki<br />

<strong>and</strong> Fukuju, 1958; Aimi <strong>and</strong> Sawamura. I959; Chapman <strong>and</strong> Peterson, 1962;<br />

<strong>and</strong> Takcshima, 1965). Others have reported thc effects <strong>of</strong> temperature on the<br />

uptake <strong>of</strong> water <strong>and</strong> nut<strong>ri</strong>ents from submerged soils (Takeshima. I964; Suzuki<br />

F. N. Ponnamperuma. Soil Chemistry Department. Intemational Rice Research Institute (IRRI). Los<br />

Bafios. Laguna, Philippines.

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