2012
DOI: 10.2136/sssaj2011.0379
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Interpreting Relationships between Soil Variables and Soybean Iron Deficiency using Factor Analysis

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Cited by 10 publications
(5 citation statements)
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“…Iron deficiency chlorosis is not related to an absence of Fe in the soil (Hansen et al, 2003). Factors such as DTPA‐extractable Fe, soluble salt concentration, carbonates in the soil, soil pH, and soil NO 3 –N can influence the incidence of IDC (Morris et al, 1990; Hansen et al, 2003; Rogovska et al, 2007; Liesch et al, 2012; Bloom et al, 2011), but in the end, IDC results from low Fe solubility preventing transport of Fe 3+ to the root surface where it is reduced to Fe 2+ to be taken up and used by the plant. In field studies, Inskeep and Bloom (1987) identified that IDC severity increased with greater concentrations of bicarbonate (HCO 3 − ) in soil.…”
mentioning
confidence: 99%
“…Iron deficiency chlorosis is not related to an absence of Fe in the soil (Hansen et al, 2003). Factors such as DTPA‐extractable Fe, soluble salt concentration, carbonates in the soil, soil pH, and soil NO 3 –N can influence the incidence of IDC (Morris et al, 1990; Hansen et al, 2003; Rogovska et al, 2007; Liesch et al, 2012; Bloom et al, 2011), but in the end, IDC results from low Fe solubility preventing transport of Fe 3+ to the root surface where it is reduced to Fe 2+ to be taken up and used by the plant. In field studies, Inskeep and Bloom (1987) identified that IDC severity increased with greater concentrations of bicarbonate (HCO 3 − ) in soil.…”
mentioning
confidence: 99%
“…redundant information was removed); moreover, effective information was integrated. Liesch et al (2011) used FA to investigate the relationships between soil variables and the incidence of iron chlorosis in seven locations in western Kansas; they obtained the best possible relationships and explained the incidence of iron chlorosis in soya beans. These results confirmed that FA can be used in large areas and several sites.…”
Section: Discussionmentioning
confidence: 99%
“…In high‐pH soils, iron is oxidized to the ferric state (Fe 3+ ), which binds tightly to anions, covalent metals, phosphorus, and soil particles and is unavailable for uptake and transport into the root in Strategy I plants (Marschner & Römheld, 1994). The relative contributions of physical and chemical soil characteristics to soybean iron deficiency have been well characterized during the past two decades (Hansen et al., 2003; Liesch et al., 2012; Robin et al., 2008). A survey of soybean fields exhibiting areas of both iron deficiency symptoms and healthy plants found that pH did not differ significantly between these areas within fields (Hansen et al., 2003), indicating that pH alone does not induce iron deficiency in soybean.…”
Section: Part I: Environmental Factors and Management Of Iron Deficiencymentioning
confidence: 99%
“…The relative contributions of physical and chemical soil characteristics to soybean iron deficiency have been well characterized during the past two decades (Hansen et al, 2003;Liesch et al, 2012;Robin et al, 2008). A survey of soybean fields exhibiting areas of both iron deficiency symptoms and healthy plants found that pH did not differ significantly between these areas within fields (Hansen et al, 2003), indicating that pH alone does not induce iron deficiency in soybean.…”
Section: Phmentioning
confidence: 99%