“…Although the movement of water through a plant is generally driven by a free energy gradient, resulting in the water column being under 'tension', positive pressure in the root system has been well documented to occur in a range of species, and is often cited in regards to monocotyledons (Fisher et al, 1997;Enns et al, 2000;Cao et al, 2012a;Gleason et al, 2017), but also in dicotyledon trees (O'Leary, 1965;Hacke & Sauter, 1996;Fisher et al, 1997), lianas (O'Leary, 1965;Fisher et al, 1997;Tibbetts and Ewers, 2000;Clearwater et al, 2007), and herbaceous species (Vaadia, 1960;Fisher et al, 1997;Stiller et al, 2003;De Swaef et al, 2013). Although the generating mechanism is yet to be identified (Pickard, 2003;Wegner, 2014), pressures range from ca 2 to 160 kPa and are known to decrease precipitously with increasing canopy transpiration and decreasing soil water potential (Fisher et al, 1997;Gleason et al, 2017).…”