4.6 Article

Evaluating Status Change of Soil Potassium from Path Model

期刊

PLOS ONE
卷 8, 期 10, 页码 -

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PUBLIC LIBRARY SCIENCE
DOI: 10.1371/journal.pone.0076712

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资金

  1. National Natural Science Foundation of China [41171243]
  2. National Key Technology RD Program [2012BAD15B01]
  3. International Plant Nutrition Institute [IPNI-HB-33]

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The purpose of this study is to determine critical environmental parameters of soil K availability and to quantify those contributors by using a proposed path model. In this study, plot experiments were designed into different treatments, and soil samples were collected and further analyzed in laboratory to investigate soil properties influence on soil potassium forms (water soluble K, exchangeable K, non-exchangeable K). Furthermore, path analysis based on proposed path model was carried out to evaluate the relationship between potassium forms and soil properties. Research findings were achieved as followings. Firstly, key direct factors were soil S, ratio of sodium-potassium (Na/K), the chemical index of alteration (CIA), Soil Organic Matter in soil solution (SOM), Na and total nitrogen in soil solution (TN), and key indirect factors were Carbonate (CO3), Mg, pH, Na, S, and SOM. Secondly, path model can effectively determine direction and quantities of potassium status changes between Exchangeable potassium (eK), Non-exchangeable potassium (neK) and water-soluble potassium (wsK) under influences of specific environmental parameters. In reversible equilibrium state of wsK reversible arrow(alpha)(beta) neK reversible arrow(gamma)(chi) eK, K balance state was inclined to be moved into beta and chi directions in treatments of potassium shortage. However in reversible equilibrium of wsK reversible arrow(epsilon)(theta) eK reversible arrow(lambda)(omega) neK, K balance state was inclined to be moved into theta and lambda directions in treatments of water shortage. Results showed that the proposed path model was able to quantitatively disclose moving direction of K status and quantify its equilibrium threshold. It provided a theoretical and practical basis for scientific and effective fertilization in agricultural plants growth.

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