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• For full-irrigation <strong>vines</strong>, there was very little change in the soil<br />

moisture below 80 cm, and soil water contents at depths of 40<br />

- 60 cm began to rewet from mid January, indicating that excess<br />

water was simply draining through the root-zone and leading to<br />

very wet subsoil<br />

• For reduced irrigation <strong>vines</strong>, soil moisture levels began to decline<br />

very soon after the irrigation treatments were imposed, even at<br />

depths below 80 cm. <strong>The</strong>re was a progressive decline in soil<br />

moisture in the top 1.4 m of soil (Figure 5). However, the full<br />

re-irrigation in early April, combined with a large rainfall event a<br />

few days earlier, resulted in rewetting and some drainage<br />

beyond 60 cm.<br />

<strong>The</strong> volume of water applied to full-irrigation <strong>vines</strong> in this trial was<br />

actually well in excess of plant requirements from mid January<br />

onwards. This over-watering resulted in increasing soil moisture<br />

levels at lower depths and the soil remained close to saturated<br />

there for virtually the entire summer period. Plant roots must<br />

acquire oxygen from soil pores for normal function and roots will<br />

become stressed if there is insuffi cient available oxygen (hypoxia),<br />

or die if soil pores are completely saturated with water, so that there<br />

is no oxygen available (anoxia). Overwatering combined with poor<br />

drainage is likely to result in root anoxia (Patterson 2004) and<br />

increases the risk that diseases such as Phytophthora root rots<br />

could occur (Max et al. 2007). <strong>The</strong>se can result in loss of root<br />

function or root death and also plant death. For example, there<br />

were signifi cant deaths of Hayward <strong>vines</strong> in 1989 in Kerikeri after<br />

very heavy rainfall, possibly as a result of anoxia (McAneney et al.<br />

1989) <strong>The</strong> absence of vine roots in deeper soil layers during soil<br />

sampling in Gisborne this year was consistent with anoxia: even if<br />

plant deaths did not occur, it is likely that plants will be less resilient<br />

to other stresses in the long term.<br />

DRY MATTER WAS INCREASED, BUT FRUIT SIZE WAS<br />

DECREASED...<br />

Applying less than full-irrigation increased fruit DM levels, but also<br />

caused a signifi cant reduction in fruit size (Table 2). For example,<br />

applying quarter-irrigation increased DM by 1.6 per cent-units, but<br />

reduced fruit weight (FW) by 8.9 g. We calculated that this would<br />

have reduced yield by c. 1,200 tray equivalents (TE) per ha. Despite<br />

the gain in TZG with this reduced irrigation, the loss of yield would<br />

have resulted in orchard gate returns (OGR) being reduced by c.<br />

$6,900/ha. Similar impacts on DM, FW and yield were observed in<br />

the half-irrigation treatments, although impacts were smaller. When<br />

we tested the impacts of different pricing mechanisms, a maximum<br />

taste payment equivalent to 120 per cent of fruit payment would<br />

have been required before the defi cit irrigation treatments would<br />

have produced a similar OGR to the full-irrigation treatment. Note<br />

that we have not included an estimate of what the reduced costs<br />

to run the irrigation would have been. Reducing the frequency of<br />

irrigation should reduce power and maintenance costs as well as<br />

reducing the environmental costs in terms of nutrient leaching.<br />

A clearance sample could have cleared fruit from the quarterirrigation<br />

treatment to be harvested about one week earlier in Week<br />

13 (26 March - 1 April) (Figure 6). In this case, the DM of fruit from<br />

the quarter-irrigation treatment would have been about 0.3 per<br />

cent-units lower but Kiwistart incentives would have been higher.<br />

Even in this scenario, there would still have been a reduced OGR<br />

Soil water content (mm/m)<br />

Figure 4. Soil sampling (top) and the installation of sap fl ow sensors (top)<br />

and time domain refl ectometry (TDR) probes (bottom) at the Gisborne<br />

orchard in 2006.<br />

Figure 5. <strong>The</strong> total amount of water stored in the top 1.4 m of the Gisborne<br />

Hayward soil profi le for full- (IR), half- (½ IR) and quarter-irrigation (¼ IR)<br />

treatments. Reduced irrigation treatments commenced on 4 January. All <strong>vines</strong><br />

were re-irrigated fully from 2 April to replicate late-season rainfall. <strong>The</strong> fi eld<br />

capacity (FC) is shown by the blue line and the permanent wilting point<br />

(WP) is shown by the grey line.<br />

compared with fully irrigated <strong>vines</strong>, but this would only have been<br />

c. $4,800/ha.<br />

<strong>The</strong> increase in DM under defi cit irrigation probably occurred via<br />

reduced dilution of carbohydrates during the starch accumulation<br />

phase of fruit growth (Richardson & Currie 2007). Although water<br />

defi cits markedly reduced fruit expansion over the summer period<br />

(22 per cent), there was a disproportionate decrease in fruit dry<br />

NZ KIWIFRUIT JOURNAL JANUARY / FEBRUARY 2008<br />

9

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