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Maclean et al. - 2002 - Rice almanac source book for the most important e

Maclean et al. - 2002 - Rice almanac source book for the most important e

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UV radiation effects<br />

UV-B radiation damages leaf tissues in rice<br />

seedlings. Leaves become stunted, stomata<br />

collapse, and photosyn<strong>the</strong>sis decreases. Some<br />

rice vari<strong>et</strong>ies appear to be b<strong>et</strong>ter able than o<strong>the</strong>rs<br />

to withstand <strong>the</strong> adverse effects of UV radiation.<br />

Leaves of tolerant vari<strong>et</strong>ies contain phenolic<br />

compounds, which are natur<strong>al</strong> chemic<strong>al</strong>s that<br />

filter out harmful UV-B radiation be<strong>for</strong>e it can<br />

damage sensitive tissues. Research is now in<br />

progress to predict possible region<strong>al</strong> losses in<br />

rice productivity if UV-B radiation continues to<br />

increase, and wh<strong>et</strong>her plant breeders can prevent<br />

those yield losses by developing new vari<strong>et</strong>ies<br />

that tolerate UV radiation.<br />

In addition to its adverse direct effects on<br />

rice plants, UV-B may change <strong>the</strong> susceptibility<br />

to and/or tolerance <strong>for</strong> disease. Although <strong>the</strong>re is<br />

no evidence y<strong>et</strong> that UV-B affects susceptibility<br />

to blast, it appears that <strong>the</strong> tolerance <strong>for</strong> blast<br />

decreases. In o<strong>the</strong>r words, UV-B does not<br />

increase disease frequency, but enhances <strong>the</strong><br />

effects of disease on plant growth.<br />

Glob<strong>al</strong> warming<br />

Although increasing atmospheric CO 2<br />

stimulates<br />

plant growth, <strong>the</strong> benefici<strong>al</strong> effects on rice<br />

growth have been observed <strong>for</strong> levels up to only<br />

500 ppm. Some plant species respond positively<br />

to CO 2<br />

levels up to 1,000 ppm. Experts predict<br />

that atmospheric CO 2<br />

will surpass 650 ppm<br />

be<strong>for</strong>e <strong>the</strong> end of <strong>the</strong> 21st century. Fur<strong>the</strong>rmore,<br />

<strong>the</strong> benefits of increased CO 2<br />

would be lost if<br />

temperatures <strong>al</strong>so rise. That is because increased<br />

temperature shortens <strong>the</strong> period over which rice<br />

grows. Research is being conducted to identify<br />

means by which rice plants may b<strong>et</strong>ter benefit<br />

from increases in atmospheric CO 2<br />

while<br />

minimizing <strong>the</strong> adverse effects of warmer<br />

temperatures (Fig. 1).<br />

Emissions of greenhouse gases<br />

from rice fields<br />

M<strong>et</strong>hane (CH 4<br />

) is second in importance to CO 2<br />

as a greenhouse gas. CH 4<br />

concentration in <strong>the</strong><br />

atmosphere has more than doubled during <strong>the</strong><br />

last 200 years. Some of this CH 4<br />

is produced by<br />

rice fields (Fig. 2). To reduce <strong>the</strong> burden and<br />

harmful effects of CH 4<br />

in <strong>the</strong> atmosphere, emissions<br />

from <strong>al</strong>l anthropogenic <strong>source</strong>s have to be<br />

mitigated.<br />

M<strong>et</strong>hane is produced in <strong>the</strong> anaerobic<br />

conditions associated with submerged soils.<br />

Much of it escapes from <strong>the</strong> soil to <strong>the</strong><br />

atmosphere via gas spaces in rice roots. The<br />

remainder bubbles up from <strong>the</strong> soil or diffuses<br />

slowly through <strong>the</strong> soil and overlying floodwater.<br />

The potenti<strong>al</strong> <strong>for</strong> CH 4<br />

emissions from rice<br />

fields has long been noted, but comprehensive<br />

measurements of CH 4<br />

fluxes in rice fields have<br />

been reported only since <strong>the</strong> early 1990s. Water<br />

regime, organic matter management,<br />

temperature, and soil properties as well as rice<br />

plants are <strong>the</strong> major factors d<strong>et</strong>ermining <strong>the</strong><br />

production and flux of CH 4<br />

in rice fields.<br />

Irrigated rice areas are <strong>the</strong> major <strong>source</strong> of CH 4<br />

emissions from rice fields. The assured water<br />

supply and control, intensive soil preparation,<br />

and resultant improved growth of rice favor CH 4<br />

production and emissions.<br />

With financi<strong>al</strong> support from <strong>the</strong> U.S.<br />

Environment<strong>al</strong> Protection Agency, IRRI<br />

undertook baseline research on CH 4<br />

fluxes in rice<br />

fields in collaboration with <strong>the</strong> Fraunhofer<br />

Institute <strong>for</strong> Atmospheric Environment<strong>al</strong> Research,<br />

Germany, and <strong>the</strong> W<strong>et</strong>land<br />

Biogeochemistry Institute of Louisiana State<br />

University, USA. O<strong>the</strong>r collaborating institutes<br />

were <strong>the</strong> Wageningen Agricultur<strong>al</strong> University,<br />

The N<strong>et</strong>herlands; <strong>the</strong> Laboratory <strong>for</strong> Microbiology,<br />

French Institute of Scientific Research <strong>for</strong><br />

Development Cooperation; <strong>the</strong> Université de<br />

Provence, France; and <strong>the</strong> University of Georgia,<br />

USA. IRRI <strong>al</strong>so coordinated an interregion<strong>al</strong><br />

research program on CH 4<br />

emissions from rice<br />

fields funded by <strong>the</strong> Glob<strong>al</strong> Environment<strong>al</strong> Facility<br />

of <strong>the</strong> United Nations Development<br />

Programme. This activity comprised<br />

collaborative CH 4<br />

research on irrigated, rainfed,<br />

and deepwater rice in China, India, Indonesia,<br />

<strong>the</strong> Philippines, and Thailand.<br />

The studies, which took <strong>al</strong><strong>most</strong> a decade of<br />

work, concluded that CH 4<br />

emissions from rice<br />

fields are much sm<strong>al</strong>ler than origin<strong>al</strong>ly thought,<br />

contributing on <strong>the</strong> order of only 10% of tot<strong>al</strong><br />

glob<strong>al</strong> CH 4<br />

emissions. High m<strong>et</strong>hane emissions<br />

are associated with specific rice management<br />

practices, and management practices can be<br />

modified to reduce emissions without reducing<br />

yields.<br />

One result was <strong>the</strong> finding that CH 4<br />

production from Indian rice production,<br />

origin<strong>al</strong>ly estimated to be some 38 million t per<br />

38 <strong>Rice</strong> <strong>al</strong>manac

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