Principles of Plant Genetics and Breeding
Principles of Plant Genetics and Breeding
Principles of Plant Genetics and Breeding
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388 CHAPTER 21<br />
duration <strong>of</strong> drought is variable, sometimes lasting for<br />
a short time <strong>and</strong> without severe adverse physiological<br />
impact, sometimes lasting throughout an entire growing<br />
season or even years, resulting in complete devastation<br />
<strong>of</strong> crops. The efforts <strong>of</strong> breeders are directed at<br />
short-duration drought that <strong>of</strong>ten is experienced when<br />
crop production is rainfed. Under rainfed conditions,<br />
rainfall is <strong>of</strong>ten erratic in frequency, quantity, <strong>and</strong> distribution.<br />
To avoid disruption in growth <strong>and</strong> development<br />
processes, <strong>and</strong> consequently in crop performance<br />
(yield), plants need to maintain a certain level <strong>of</strong> physiological<br />
activity during the adverse period.<br />
The effect <strong>of</strong> drought varies among species <strong>and</strong> also<br />
depends on the stage <strong>of</strong> plant growth <strong>and</strong> development<br />
at which the moisture stress occurs. Drought at flowering<br />
may cause significant flower drop <strong>and</strong> low fruit set.<br />
Similarly, when drought occurs at fruiting, there will<br />
be fruit drop <strong>and</strong>/or partially filled or shriveled fruits.<br />
In the end, both quality <strong>and</strong> product yield will be<br />
decreased.<br />
Overview <strong>of</strong> drought stress concepts<br />
Scientists have developed crop simulation models that a<br />
researcher may use to estimate <strong>and</strong> quantify the impact<br />
<strong>of</strong> specific drought stress conditions on crop productivity.<br />
Models are available for cereals (e.g., maize, wheat,<br />
rice), grain legumes (e.g., soybean, dry bean, peanut),<br />
root crops (e.g., cassava, potato), <strong>and</strong> other crops<br />
(e.g., tomato, sugarcane).<br />
As the dem<strong>and</strong> for water exceeds supply, a plant<br />
develops what is called plant water deficit. The supply<br />
<strong>of</strong> water is determined by the amount <strong>of</strong> water held<br />
in the soil to the depth <strong>of</strong> the crop root system. The<br />
dem<strong>and</strong> for water is determined by plant transpiration<br />
rate or crop evapotranspiration (both plant transpiration<br />
<strong>and</strong> soil evaporation). The rate <strong>of</strong> transpiration is<br />
influenced by solar radiation, ambient air temperature,<br />
relative humidity, <strong>and</strong> wind. These factors control transpiration<br />
at the single leaf level. The most important<br />
factor that controls transpiration at the whole-plant or<br />
crop level is total leaf area.<br />
It is difficult to sense <strong>and</strong> estimate plant water stress<br />
at whole-crop levels because <strong>of</strong> the need to integrate<br />
an estimate based on the whole canopy. Various plantbased<br />
methods are used to obtain direct measurements<br />
<strong>of</strong> water status, stress status, <strong>and</strong> other physiological<br />
consequences <strong>of</strong> water deficit. These include leaf water<br />
potential, relative water content, <strong>and</strong> osmotic potential.<br />
Soil moisture is measured in a variety <strong>of</strong> ways. The soil<br />
moisture content (volume) is measured by gravimetric<br />
methods (soil is weighed before <strong>and</strong> after drying to<br />
determine water content). The soil water status is measured<br />
in terms <strong>of</strong> potential <strong>and</strong> tension. The amount<br />
<strong>of</strong> water a given crop can extract from the soil at a<br />
given water potential <strong>and</strong> depth is called the extractable<br />
soil moisture. Most crops usually extract between<br />
50% <strong>and</strong> 80% <strong>of</strong> the extractable soil moisture before<br />
crop transpiration is reduced <strong>and</strong> symptoms <strong>of</strong> water<br />
deficit occur.<br />
The relative importance <strong>of</strong> the major mediators <strong>of</strong><br />
cellular response to water deficit are not exactly known.<br />
<strong>Plant</strong> hormones (e.g., abscisic acid) are believed to be<br />
a key factor in water stress response. Numerous water<br />
stress responsive genes have been identified. At the<br />
whole-plant or crop level, water deficit effects manifest<br />
in various ways – phenology, phasic development,<br />
growth, carbon accumulation, assimilate partitioning,<br />
<strong>and</strong> reproductive processes. These manifestations are<br />
primarily responsible for the variations in crop yield<br />
attributable to drought stress. Water deficit causes<br />
reduced cell expansion, reduced plant water use, <strong>and</strong><br />
reduced plant productivity. Reduced cell expansion<br />
also adversely impacts meristematic development <strong>of</strong><br />
yield components (e.g., inflorescence or tiller initials in<br />
cereals), leading to potentially small reproductive<br />
organs <strong>and</strong> hence reduced yield. Damage to the meristem<br />
is usually irreversible <strong>and</strong> cannot be corrected by<br />
irrigation. Water deficit also causes advanced or delayed<br />
flowering, depending on the species. This alteration in<br />
phasic development is known to be critical to maize<br />
yield under stress. Water deficit can cause reproductive<br />
failure whereby the pollen may desiccate, creating an<br />
effect similar to male sterility, <strong>and</strong> leading to reduced<br />
grain set. The duration <strong>of</strong> grain filling is reduced under<br />
stress. The root : shoot dry weight ratio increases as<br />
plants slip into water stress.<br />
Managing drought stress<br />
Irrigation is the primary means <strong>of</strong> addressing drought in<br />
crop production, provided this approach is economical.<br />
Crop production may be designed for irrigated or dryl<strong>and</strong><br />
(rainfed) environments. In irrigated production,<br />
the common practice is to implement a supplemental<br />
irrigation regime, whereby irrigation is applied when<br />
rainfall is inadequate. Various soil <strong>and</strong> water conservation<br />
practices may be adopted to conserve soil moisture<br />
from one season to another. Practices such as fallow<br />
<strong>and</strong> the use <strong>of</strong> ground cover are recommended practices<br />
for soil <strong>and</strong> water conservation.