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4. DEVELOPMENT AND APPLICATION OF<br />

BIOFERTILIZERS IN THE REPUBLIC OF CHINA<br />

Dr. Chiu-Chung Young<br />

Department of Soil and Environmental Sciences<br />

National Chung-Hsing University<br />

Taichung, Republic of China<br />

INTRODUCTION<br />

Taiwan experiences a humid, subtropical climate, with a mean temperature of around 20°C<br />

(November to April) and above 30°C (June to November). Rainfall is over 3,000 mm in the central<br />

region, 1,500–3,000 mm on the east coast, and 1,500–2,000 mm in the western region adjacent<br />

to mountains, with frequent typhoons during summer and autumn impacting agriculture.<br />

Uncontrolled application of chemical fertilizer is a common practice in most areas. The estimated<br />

consumption of chemical fertilizer is about 1,140,000 tons <strong>for</strong> 844,000 ha. However,<br />

many upland regions and lowland soils are less fertile and need greater fertilizer input to sustain<br />

yields.<br />

Agriculture is oriented towards intensive farming practices, and every ef<strong>for</strong>t is being made<br />

to shorten the growth period of each crop so that more crops can be grown during the following<br />

season. Intensive multiple cropping systems have drastically reduced the use of leguminous<br />

plants as green manure, since this requires a longer growth period. Still, legumes such as soybean,<br />

peanut, mungbean, pea, etc. are planted, but only as part of an intensive multiple cropping<br />

system (Young and Chao, 1983).<br />

It is well known that the crop root zone (rhizosphere) provides a unique microsite <strong>for</strong> the<br />

association of symbiotic and nonsymbiotic microorganisms (Young, 1994). N2-fixing and Psolubilizing<br />

bacteria have been well characterized from various soil types and aquatic environments<br />

(Seshadri et al., 2000; Garg et al., 2001; Berman-Frank et al., 2001; Young et al., 1982;<br />

Young and Cheng, 1998; Young et al., 2003a,b&c), and many isolates have been shown successful<br />

in improving crop yield (Subba Rao, 1982; Young et al., 1988a&b; Young, 1994). Hence,<br />

several beneficial microorganisms can be used effectively as a chemical fertilizer alternative to<br />

minimize the application of inorganic fertilizers.<br />

Biofertilizers, which can be more appropriately called microbial inoculants, can be generally<br />

defined as preparations containing live or latent cells of an efficient microbial strain capable<br />

of nitrogen-fixing, phosphate-solubilizing (bacteria, fungi, or algae), or any other beneficial<br />

activity derived from this process. Biofertilizers may be applied to either seed or soil to accelerate<br />

microbial processes in soil, thereby augmenting the availability of nutrients by making<br />

them easily assimilated by crop plants.<br />

This paper briefly reviews the status of biofertilizers that have been developed in a few Republic<br />

of China laboratories in recent years, with a major emphasis on microorganisms, including<br />

rhizobium, P-solubilizing bacterium, and mycorrhizal fungi that were identified as suitable<br />

candidates able to meet the nutrient requirements of various crop species and known to increase<br />

yields.<br />

SELECTION AND DEVELOPMENT OF BIOFERTILIZERS<br />

Rhizobial Inoculants<br />

In the Republic of China, research on the selection of efficient rhizobial strains <strong>for</strong> inoculation<br />

started in 1958. Collection, isolation, and subsequent selection of effective rhizobial strains<br />

and their uses in agriculture have yielded fruitful results. Since marked variations were observed<br />

– 51 –

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