Phosphate toxicity and iron deficiency

Bert’s post yesterday reminded me of some work one of my graduate students did about 10 years ago.  We were curious to see whether a transplant fertilizer containing phosphate was correlated with foliar iron deficiency, which is visualized as interveinal chlorosis:

 What Scott did was to plant 10 rhododendrons per treatment into pots containing containing a name brand azalea, camellia and rhododendron food (5-5-3) at 0, 0.5, 1.0, and 2.0 times the recommended amount. Here are some of the results of that study:

 
Total number of chlorotic plants

Total foliar iron vs. fertilizer treatment

Chlorosis as a result of phosphate fertilizer. 1= Normal (green leaves), 2= Light chlorosis in young leaves, 3= Moderate chlorosis, 4= Severe chlorosis, young leaves white

 For gardeners, the take home message might be that the control plants – those without any transplant fertilizer added – did the best. Don’t add phosphate to your landscape and garden soils unless you have a verified deficiency.  And only a soil test will tell you this conclusively.

You can’t fly by the seat of your pants on this one, folks.

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Linda Chalker-Scott

Dr. Linda Chalker-Scott has a Ph.D. in Horticulture from Oregon State University and is an ISA certified arborist and an ASCA consulting arborist. She is WSU’s Extension Urban Horticulturist and an Associate Professor in the Department of Horticulture, and holds two affiliate associate professor positions at University of Washington. She conducts research in applied plant and soil sciences, publishing the results in scientific articles and university Extension fact sheets. Linda also is the award-winning author of five books: the horticultural myth-busting The Informed Gardener (2008) and The Informed Gardener Blooms Again (2010) from the University of Washington Press and Sustainable Landscapes and Gardens: Good Science – Practical Application (2009) from GFG Publishing, Inc., and How Plants Work: The Science Behind the Amazing Things Plants Do from Timber Press (2015). Her latest effort is an update of Art Kruckeberg’s Gardening with Native Plants of the Pacific Northwest from UW Press (2019). In 2018 Linda was featured in a video series – The Science of Gardening – produced by The Great Courses. She also is one of the Garden Professors – a group of academic colleagues who educate and entertain through their blog and Facebook pages. Linda’s contribution to gardeners was recognized in 2017 by the Association for Garden Communicators as the first recipient of their Cynthia Westcott Scientific Writing Award. "The Garden Professors" Facebook page - www.facebook.com/TheGardenProfessors "The Garden Professors" Facebook group - www.facebook.com/groups/GardenProfessors Books: http://www.sustainablelandscapesandgardens.com

11 thoughts on “Phosphate toxicity and iron deficiency”

  1. I agree with the genral comment that the fertilizer is not required and seems to cause some chlorosis. However, I don’t see the data that puts the blame on excess phosphate?

  2. Robert, this was just a smidgen of the data we generated. The only differences among treatments were the levels of fertilizer used. Neither nitrogen nor potassium interferes with iron uptake – but phosphate does. (I think I’ve blogged about this interference before, but I probably should have repeated that bit.)

  3. Any ideas of what to do when you’ve bought land where all of the plants have this issue because the previous owner added way too much fertilizer?

  4. Terri, they died before the end of the experiment. So we didn’t count them (though that would have made the results even more spectacular). Jen, sorry I didn’t see your older message – but you can plant a cover crop to draw down the nutrients. Remove the cover crop and compost or discard, but don’t till it back in. You will have to add back nutrients like nitrogen.

  5. Jacquie, it appears to compete with iron for binding sites at the cellular level. The more phosphorus, the less chance iron has to be bound and taken up by the roots.

    1. It’s actually a salt metathesis (double-displacement) reaction that happens in the soil, causing the iron to become an insoluble precipitate. When iron ions come into contact with phosphate ions, they form iron phosphate, which has practically no solubility. It’s just like the classic high school chemistry experiment where a solution of sodium carbonate is added to a solution of copper sulfate, and a precipitate of copper carbonate forms.

      (I am currently studying chemistry as a college student, and my biggest hobbies are gardening and plant propagation)

        1. Makes sense, since plant roots take up nutrients primarily by ion exchange*, but nothing says that at any given time, the plant can only take up anions or cations. They can take up both, so long as they are replaced with H+ and OH- accordingly. Since the iron doesn’t normally immobilize until it is converted to chlorophyll, which is the whole reason the plant needs it, in order for that, the iron needs to remain soluble up until then. When there’s too much phosphate, however, the iron immobilizes prematurely, so the chlorophyll isn’t getting made, and the plant goes chlorotic.

          *When they take up nutrient cations, they do so by replacing each unit of positive charge with a H+ ion, which is obviously another cation, but when they take up anions (like phosphate), they replace each unit of negative charge with a OH- ion, which is obviously another anion.

          For cations:
          For each NH4+ ion the plant takes from the soil, one H+ is returned in its place. For each Fe+2, Mg+2, Ca+2, Zn+2, Mn+2, Cu+2, and Ni+2 ion the plant takes from the soil, two H+ ions are added to the soil to equalize charge.

          For anions:
          For each NO3- ion taken up by a plant, one OH- is added to the soil to equalize charge.
          For each PO4 -3 ion taken up, three OH- ions are used to equalize charge.

          1. You’re looking at this from strictly a soil chemistry perspective. What you need to add is the influence of both roots and mycorrhizae, which acidify the rhizosphere and enable metal solubilization. The problem for plants is the competition for membrane uptake sites – not soil immobilization.

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