04.06.2016 Views

Yoshida - 1981 - Fundamentals of Rice Crop Science

Yoshida - 1981 - Fundamentals of Rice Crop Science

Yoshida - 1981 - Fundamentals of Rice Crop Science

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

GROWTH AND DEVELOPMENT OF THE RICE PLANT 37<br />

1.35. Water extraction patterns after the irrigation on 21 Mar 1978 (IRRI 1979).<br />

to the effective total root length if other conditions are held constant (Gardner<br />

1960, 1964).<br />

The high rate <strong>of</strong> water absorption results in a more rapid decrease in soil water<br />

potential in the shallow layers. Since the rate <strong>of</strong> water absorption is also proportional<br />

to soil water potential if other things are the same, the water absorption from<br />

the shallow layers will decrease. At this time, more water is available to the roots<br />

in the deeper soil pr<strong>of</strong>iles, and, hence, more water will be absorbed from these<br />

layers.<br />

In the mathematical model presented by Gardner (1960), the root was considered<br />

an infinitely long cylinder <strong>of</strong> uniform radius and water-absorbing properties.<br />

That is an approximation <strong>of</strong> the plant’s root and may not always apply to the real<br />

root. For greater accuracy, the root length should be corrected for root hairs and for<br />

degree <strong>of</strong> suberization.<br />

The total root length is also related to the plant’s capacity to absorb a nutrient.<br />

For corn plants grown in culture solution, the rate <strong>of</strong> phosphate uptake was<br />

proportional to the total root length (Jungk and Barber 1974). Thus, the capacity<br />

<strong>of</strong> the plant to absorb water and nutrients is closely related to the total length <strong>of</strong> the<br />

root system.<br />

1.7.6. Measurement <strong>of</strong> root length and root density<br />

Measurement <strong>of</strong> total root length, even in a small sample, is difficult and tedious<br />

because roots can reach great lengths in even small volumes <strong>of</strong> soil. In 1966,<br />

Newman devised an elegant technique by which the total root length can be<br />

measured with relative ease. Newman’s method, as it is popularly used, uses a grid<br />

over which a root is randomly spread (Marsh 1971). Consider a grid with a total<br />

area <strong>of</strong> 14 × 14 cm 2 and with a regular distance <strong>of</strong> 14/11 cm between lines (Fig.<br />

1.36). It is expected that the longer the root that is spread on the grid, the more<br />

intercepts it will make with the straight lines. Thus, the number <strong>of</strong> intercepts can be

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!