A variety of fluid transport phenomena in plants do not require active pumping or externally imposed pressure difference to move solutes and fluids. Instead, they rely on osmotic pressure, a passive transport process, to move loaded solutes and water simultaneously. A prototypical example is sucrose transport in the phloem of plants formulated in the 1930s by Ernst M 𝐴𝐴 𝐴 u nch and is now labeled as the pressure-flow hypothesis (Münch, 1930) or pressure flow hypothesis (PFH) (van Bel, 2003). The PFH is routinely used to describe the transport of photosynthates from production sites (leaves) to areas of consumption or storage (growing tissues and roots). This mechanism has been used to explain aspects of plant mortality under extreme weather conditions (Sevanto et al., 2014) and ecosystem-scale impacts on carbon and water cycling (Nikinmaa et al., 2013), which is why it continues to be a subject of active research in eco-hydrology (