Название: Wheat
Автор: Peter R. Shewry
Издательство: John Wiley & Sons Limited
Жанр: Биология
isbn: 9781119652595
isbn:
The environment clearly has an impact on wheat supply and, conversely, wheat influences the environment. If we are to address the sustainability of wheat production, both factors need to be understood. Our current reliance on cereal grain, and on wheat in particular, has significant implications for human health and well‐being. The relationships between wheat production, the environment, and human diet and health are therefore the overarching themes of this book.
For the remainder of this chapter, we will introduce three of the main factors that account for the global success of the wheat crop. Firstly, the wheat plant is described in terms of its growth and development as a grass. Secondly, we introduce the evolution of wheat and explain its wide adaptability. Finally, we introduce the unique processing properties of wheat and the diversity of wheat grain types and wheat‐based products.
1.2 The Wheat Plant
As already said, wheat, like other cereals, is a grass plant grown primarily for its edible seed. The lineages of wheat, rice, and maize may have diverged from a common ancestor about 40 MYA (Huang et al. 2002; Gill et al. 2004). The wheats (Triticum spp.) form part of the Triticeae tribe, which also includes closely related cereals, notably barley ( Hordeum vulgare ) and rye ( Secale cereale ), as well as many wild grasses, such as the weed common couch grass ( Elymus repens ). The lineages of wheat and barley appear to have separated 10–14 MYA, and of wheat and rye 7 MYA.
Table 1.2 Köppen climate classifications used in Figure 1.6.
Source: adapted from Peel et al. (2007).
Grouping | Water distribution | Temperature description | Composite classification |
---|---|---|---|
B Desert/semi‐arid | |||
S Semi‐arida | |||
k coldb | BSk | ||
C Temperate/mesothermalc | |||
s Dry summerd (Mediterranean) | |||
a Hot summere | Csa | ||
w Dry winterf (e.g. subtropical) | |||
a Hot summere | Cwa | ||
f No dry season (e.g. oceanic) | |||
b Warm summerg | Cfb | ||
D Continental/microthermalh | |||
w Dry winterf | |||
a Hot summere | Dwa | ||
f No dry season | |||
a Hot summere | Dfa | ||
b Warm summerg | Dfb |
Definitions:
a ‘Semi‐arid’ is where the mean annual precipitation is > 5× but < 10 × a threshold precipitation. When precipitation is relatively evenly distributed, the threshold precipitation is 2 × mean annual temperature (°C) +14.
b ‘Cold’ is where mean annual temperature is < 18 °C.
c ‘Temperate’ is where the mean temperature of the hottest month is > 10 °C and the coldest month is between 0 and 18 °C.
d A ‘dry summer’ is where the precipitation in the driest summer month is < 40 mm and also less than a third of the wettest month in winter.
e A ‘hot summer’ is where the mean temperature of the hottest month is ≥ 22 °C.
f A ‘dry winter’ is where the wettest winter month has less than a tenth of the precipitation than the wettest summer month.
g A ‘warm summer’ is where the hottest month is < 22 °C but there are at least four months where the mean temperature is > 10 °C.
h A continental climate is where the hottest month is > 10 °C but the coldest month is ≤ 0 °C.
The Triticeae have common structures and patterns of development typical of many grasses. It is normal to define phases of development in terms of growth stage scores (Table СКАЧАТЬ