There are essentially two main types of irrigation; primary irrigation, which is needed for areas (such as very dry climates) that lack sufficient rainfall for viticulture to even exist, and supplemental irrigation where irrigation is used to "fill in the gaps" of natural rainfall to bring water levels to better numbers as well as to serve as a preventive measure in case of seasonal drought conditions. In both cases, both the climate and the
vineyard soils of the region will play an instrumental role in irrigation's use and effectiveness. - the period that includes flowering and fruit set, when the water is most crucial. While fluctuations in rainfall do occur, the amount of natural precipitation, combined with water holding capacity of soil, is typically sufficient to result in healthy harvest. In contrast,
Napa Valley only gets 2.4 inches (60 mm), on average, during the same period of time, often in an erratic pattern (some years seeing more, some years seeing only trace amounts of rain), and most appellations in Central and Southern California (both along the coast and inland) receive even less than that, necessitating supplemental irrigation. Continental climates are usually seen in areas further inland from the coastal influences of oceans and large bodies of water. The difference from the average mean temperature of its coldest and hottest months can be quite significant with moderate precipitation that usually occurs in the winter and early spring. Depending on the water retaining ability of the soil the grapevine may receive enough water during this period to last throughout the growing season with little if any irrigation needed. For soils with poor water retention, the dry summer months may require some supplemental irrigation. Examples of continental climates that use supplemental irrigation include the
Columbia Valley of
Washington State and the
Mendoza wine region of
Argentina. Water retention refers to the soil's ability to hold water. The term "field capacity" is used to describe the maximum amount of water that deeply moistened soil will retain after normal drainage. Drainage is the ability of water to move freely throughout the soil. The ideal circumstance is soil that can retain sufficient amount of water for the grapevine but drains well enough to where the soil doesn't become
water-logged. Soil that doesn't retain water well encourages the vine to easily sleep into water stress while soil that doesn't drain well runs of the risk of water-logged roots being attacked by
microbial agents that consume all the soil nutrients and end up starving the vine. The
depth,
texture and
composition of soils can influence its water retaining and draining ability. Soils containing large amounts of
organic material tend to have the highest water retention abilities. These types of soils include deep
loams,
silty soils like what is typically found on the fertile valley floors such as in the California's
Napa Valley.
Clay particles have the potential to remain in
colloidal suspension for long periods of time when it is dissolved in water. This gives clay-based soils the potential to retain significant amount of water such as the clay soils of the
Right bank Bordeaux region of
Pomerol. Many regions with these types of water retaining soils have little need for irrigation, or if they do it is usually supplemental during periods of drought. Soils with poor water retention include
sand and
alluvial gravel based soils such as those found in the
Barolo and
Barbaresco zones of
Italy or in many areas of
South Australia. Depending on the climate and amount of natural rainfall, areas with poor water retention may need irrigation. Just as having too little water is detrimental to the grapevine, so too is having too much. When vines become water-logged they become a target for various microbial agents such as
bacteria and
fungi that compete with the vine for nutrients in the soil. Additionally excessively moist soil is poor conductor of valuable heat radiating from the ground. In general wet soils are cold soils which can be especially problematic during the
flowering causing poor berry set that could lead to
coulure. It also becomes an issue during the ripening stage when vines in cool-climate regions may need additional heat radiated from the ground in order to sufficiently ripen its fruit (an example of this is the
slate-based vineyards of the
Mosel in
Germany). Therefore, well draining soils are considered very conducive to producing quality wine. In general light-textured (such as sand and gravel) and stony soils tend to drain well. Soils heavy soils and those with high proportions of organic matter also have the potential to drain well if they having a crumbling texture and structure. This texture relates to the
friability of the soil which can come from
earthworms and other organisms that have burrowed tunnels throughout the soil. Much like rocks, these tunnels give water a freer passageway through soil and contributes to its drainage.
Measuring soil moisture Because of the problems associated with water-logged and wet soils, it is important for viticulturist to know how much water is currently in the soil before deciding if and how much to irrigate. Nowadays, precision agriculture uses high technology in the field, providing the producers with accurate measurements of the water needs of any specific vine. There are several methods of evaluating soil moisture. The most basic is simple observation and feeling of the soil, however this has its limitations since the
subsoil may be moist while the
surface soil appears dry. More specific measurements can be attained by using
tensiometers which evaluates
surface tension of water extracted from the soil. The presence of water in the soil can be measured by
neutron moisture meters that utilize an
aluminium tube with an internal neutron source that detect the subtle change between the water in the soil. Similarly,
gypsum block placed throughout the vineyard contain an
electrode that can be used to detect the electrical resistance that occurs as the soil dries and water is released by evaporation. Since the 1990s there has been greater research into tools utilizing
time-domain reflectometry and
capacitance probes. In addition to monitoring for excessive moisture, viticulturists also keep an eye for signs of water stress (discussed below) due to severe lack of water. ==Irrigation systems==