Abstract
Twenty‐five sorghum [Sorghum bicolor (L.) Moench cv GP‐10] seed were planted in ‘white quartz flintshot’ sand and grown for four days. Root tips (1 cm), washed from the sand, were exposed to p‐chloromercuribenzene (PCMB) (1 mM) or p‐chloromercuribenzene sulfonic acid (PCMBS) (1 mM) plus 45Ca2+ (0.1 μCi) at pH 6.0, 5.5, 5.0, 4.5, or 4.0. In untreated roots, 45Ca uptake decreased as H+ concentration increased. PCMBS is membrane impermeant and inactivates exofacial sulfhydryl groups (SH). PCMB is lipid soluble and inactivates SH at the surface and inside of the root plasma membrane. Ion channel 45Ca uptake (+ PCMBS) was greater than 45Ca uptake in untreated roots at pH 6.0, 5.5, and 5.0, indicating 45Ca efflux by Ca2+‐ATPases was maximized at pH 6.0 and decreased as H+ concentration increased. With PCMB treatment, ion channel 45Ca uptake was less than the untreated 45Ca uptake at pH 6.0 and 5.5 (2‐hr exposure). But at pH 4.5, 45Ca uptake by ion channels (+ PCMB) was greater than 45Ca uptake (pH 6.0) of the untreated roots. GP‐10 was selected for growth on low pH soil and for metolachlor tolerance. Therefore, genetic variation due to selection has resulted in ion uptake modes that are considerably different within the species.