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Vergara - 1976 - Physiological and morphological adaptability of ri

Vergara - 1976 - Physiological and morphological adaptability of ri

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TENIPERATTIRE AND truss-nest. Kinetics or FLOODED sorts 251<br />

Ctilibqulflfl sway locrr. LUISlEIW zlcy LID-Y‘ 9115- I'm<br />

1. Influence <strong>of</strong> temperature on the kinetics <strong>of</strong> pH in three soils.<br />

9.5%; free Fe: 0.1%); it was least in a calcareous clay loam (pH: 7.6‘. organic<br />

matter: 1.5%; free Fe: 0.3%). The acid sulfate soil attained a pH <strong>of</strong>4.l (the pH<br />

above which aluminum toxicity disappears) within a week <strong>of</strong> flooding at 25°C:<br />

at 15°C it took 10 weeks. A later study <strong>of</strong> the influence <strong>of</strong> temperature regimes<br />

similar to those obtaining in <strong>ri</strong>ce fields in four typical locations (Cho <strong>and</strong> Ponnamperuma.<br />

1971) confirmed the marked retardation <strong>of</strong> pH increase in Luisiana<br />

clay <strong>and</strong> in another acid soil Casiguran s<strong>and</strong>y loam (pl-l 1 4.9‘. O.M.: 5.3%; free<br />

Fe: 0.35%). by low temperature (Fig. l). It also showed that in Libon silt loam<br />

(pl-l; 5.9". organic matter: 4.0%; Tree Fe: 0.1%) the temperature effect was not<br />

appreciable.<br />

The slow increase in p11 may be one factor retarding the growth Offillfi on cold<br />

acid soils.<br />

Specific conductance<br />

Temperature affects the kinetics <strong>of</strong> specific conductance through its effects on the<br />

production <strong>of</strong> water-soluble ions such as Fe“, Mn”. NPLfl HCO} <strong>and</strong> the<br />

removal <strong>of</strong> Fe='. Mn“ as precipitates <strong>of</strong> Fe,O, -nH2O <strong>and</strong> MnCO, Thus the<br />

changes in specific conductance roughly parallel those <strong>of</strong> iron <strong>and</strong> manganese.<br />

In a study <strong>of</strong> eight soils at 15°. 25°, 35°. <strong>and</strong> 45°C. peak values were highest<br />

in most soils at 45°C (IRRI. 1967). Some <strong>of</strong> these values exceeded 4 minho/cm.<br />

the level above which <strong>ri</strong>ce suffers from salt inj ur_v.<br />

CHEMICAL KINETIC S<br />

Carbon dioxide<br />

Carbon dioxide plays an important role in ionic equilib<strong>ri</strong>a in flooded soils. Its<br />

partial pressure (Ptfog determines the pI-I. Eh, <strong>and</strong> the solubility <strong>of</strong> iron, manganese.<br />

<strong>and</strong> calcium in flooded soils (lRRL 1966). If PCO, is too large, the concentration<br />

<strong>of</strong> Fe" may reach toxic levels <strong>and</strong> in addition CO, may directly‘<br />

poison the plant; if too low. the pH increases <strong>and</strong> this lowers the concentrations<br />

<strong>of</strong> Fe='_ so the plant may suffer from iron injury.

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