According to FAO,
worldwide agriculture accounts for over 70% of blue water consumption. The
anticipated future increase in global population, from 6.1 billion people in
2000 to 8.9 billion by 2050, entails the increase of agricultural production.
It is estimated that by 2030 50% more food has to be produced, and twice the
current amount of food by 2050. However, this increase in food production
should be carried out with the least amount of water needed, mainly due to increases
in urban and industrial water consumption and possible consequences of climate
change. It will be necessary to increase the water needed for food production
from the current 7.000 km3 to 9.000-11.000 km3 by 2050.
Spain is no exception, water
consumption is strongly geared towards the agricultural sector, and the rate of
exploitation of renewable resources exceeds 30%. In the past 20 years, the
irrigated area has raised to 20%, causing a large increase in water demand.
This makes Spain the country with the largest irrigated area in Europe, with
nearly one third of the total European irrigated area. Nevertheless, Spain
remains a net importer of virtual water, with more than 25,000 million m3
per year, mainly associated with the import of cereals and industrial crops
such as soybeans or cotton. But more and more criticism arises against the
agriculture sector remaining the centre stage. The old paradigm "more
crops and jobs per drop" is shifting towards “more cash and nature per
drop". Determining the current and future water demands will help to
implement sustainable policies for water resources management.
Water use at a
national level has traditionally been measured by indicators such as water
withdrawal, which only considers the total freshwater used by a country in its
production system. The use of indicators such as the Water Footprint (WF)
allows analysing not only the impacts generated at the national level, but all
those associated with the consumption of goods produced abroad. This
multidimensional indicator distinguishes also between blue water (surface and
groundwater) and green water (water from rain accumulated in the soil).It is
furthermore possible to quantify the impact of pollution by calculating the
gray water, which is defined as the total freshwater required to assimilate the
load of pollution.
The Virtual Water
(VW) concept was defined by professor Tony Allan in the beginning of the 90´s;
since then, notable advances in the development of the Water Footprint concept
have been achieved. The first major quantification of water flows associated
with trade of commodities was made by Chapagain and Hoekstra. They established
the VW flows of several crops and derived products. Nowadays, this methodology
is standard, thanks to the efforts of the researchers of the Water Footprint
Network. Methodological advances include the use of complex geographical models
to estimate the water use of crops (CWU)(Mekonnen and Hoekstra, 2011; 2012). These models are
based on water balances equations. They allow for the estimation of the amount
of water embedded in crops in a certain area and at a given time.
Water balance models can be developed at different
time and spatial scales, thus they vary in complexity and input data. There are several models to calculate crop water
requirements on a global scale. Some of the most recent ones have been
implemented with a resolution of 5 minutes and a
total of 26 crop classes (both for rainfed and irrigated conditions). Some
other models have been was applied to 126 crops, including calculations of gray
water. But, the certainty of these models is influenced by the input data:
location of crops and planting dates, weather variables, soil properties, etc. The total available water capacity of the soil (TAWC) plays a critical role in determining the overall
water balance because it acts as a water reservoir.
To sort out some of
such drawbacks researchers (A. de Miguel, M. Kallache and E. García-Calvo) have
developed a spatial crop water use model (CWUModel), which computes the Water
Footprint of agriculture in the Duero river basin. This model enables daily
water balances in a geospatial context, distinguishing between green water and
blue water.
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