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494                                      Frutas del trópico







                    Calcareous soils:
               The definition of calcareous soils by the Soil Science Society of America: soil containing suffi-

               cient free CaCO  and other carbonates to effervesce visibly or audibly when treated with cold
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               0.1M HCl. These soils usually contain from 0.1 to almost 100% CaCO . Therefore, both
                                                                                              3
               Krome very gravelly loam and Chekika very gravelly loam are also classified as calcareous

               soils because they were derived from Miami limestone and usually contains from 30 to 90%

               CaCO . The pH values of calcareous soils are greater than 7, usually in the range of 7.4-8.4.
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               Textures of calcareous soils can be sandy, loamy or gravelly. Soil depths range from less than 10

               cm to over a meter. These soils are important for production of tropical fruit in Florida. Over

               85% of Florida’s tropical fruits are grown on calcareous soils in the southern part of the state.
               This is done because of favorable temperatures, rather than favorable soil characteristics. Ca-

               reful management of nutrients is critically important to the successful production of crops on

               calcareous soils.


                    Nutrient management for calcareous soils

                    Grow crop tolerant to calcareous soils:

               Growing high-pH tolerant crops is a useful management option for coping with calcareous soils.

               Plants show chlorosis usually on soils higher than 20% Ca content and has been a problem

               since the first commercial tropical fruit groves were established in South Florida. The chlorosis

               is mainly nutrient deficiency, especially Fe. Roots of Fe-efficient plants react to Fe-deficiency
               stress by strongly enhancing reductase activity, lowering the rhizosphere pH with excretion of

               H+, and releasing acids that act as chelates.  Those characteristics make it possible to select

               Fe-efficient genotypes.  So far there is no research report on this topic.












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