A method was established for the determination of elemental S (So) in soils. The So added to four arable soils was extracted with chloroform, digested with fuming HNO3KNO3 and determined using inductively coupled plasma atomic emission spectroscopy (ICP-AES). The method gave recoveries of between 96.6 and 100.4% in air-dried soils and in the same soils at 50% of the water holding capacity (WHC), with CVs varying between 0.4 and 5.6%. Complete recoveries were also obtained at soil moisture contents of 2 and 4 times of WHC, although precision was poorer. In contrast, the digestion method using HClO4HNO3 was not suitable, because it resulted in only about 80% recovery of So. An incubation study showed that the net amount of sulphate-S produced was substantially less than the decrease of So in four soils. After 38 days of incubation at 25°C, the percentages of total oxidised S appearing as sulphate-S were greater in the two sandy soils (64–78%) than in the two clayey soils (34–40%). The difference between the oxidation of So and the production of sulphate-S was probably due to microbial immobilisation. It is suggested that both measurements are needed to study the oxidation of So in soils and the availability of oxidised S to crops.
No abstract is provided for this article.
No abstract is provided for this article.
No abstract is provided for this article.
No abstract is provided for this article.
Molybdenum (Mo) is an essential element for almost all living organisms. After being taken up into the cells as molybdate, it is incorporated into the molybdenum cofactor, which functions as the active site of several molybdenum-requiring enzymes and thus plays crucial roles in multiple biological processes. The uptake and transport of molybdate is mainly mediated by two types of molybdate transporters. The homeostasis of Mo in plant cells is tightly controlled, and such homeostasis likely plays vital roles in plant adaptation to local environments. Recent evidence suggests that Mo is more than an essential element required for plant growth and development; it is also involved in local adaptation to coastal salinity. In this review, we summarize recent research progress on molybdate uptake and transport, molybdenum homeostasis network in plants, and discuss the potential roles of the molybdate transporter in plant adaptation to their local environment.
Uptake of Cd and Zn by intact seedlings of two contrasting ecotypes of the hyperaccumulator Thlaspi caerulescens was characterized using radioactive tracers. Uptake of Cd and Zn at 2 °C was assumed to represent mainly apoplastic binding in the roots, whereas the difference in uptake between 22 °C and 2 °C represented metabolically dependent influx. There was no significant difference between the two ecotypes in the apoplastic binding of Cd or Zn. Metabolically dependent uptake of Cd was 4.5‐fold higher in the high Cd‐accumulating ecotype, Ganges, than in the low Cd‐accumulating ecotype, Prayon. By contrast, there was only a 1.5‐fold difference in the Zn uptake between the two ecotypes. For the Ganges ecotype, Cd uptake could be described by Michaelis–Menten kinetics with a Vmax of 143 nmol g−1 root FW h−1 and a Km of 0.45 μM. Uptake of Cd by the Ganges ecotype was not inhibited by La, Zn, Cu, Co, Mn, Ni or Fe(II), and neither by increasing the Ca concentration. By contrast, addition of La, Zn or Mn, or increasing the Ca concentration in the uptake solution decreased Cd uptake by Prayon. Uptake of Ca was larger in Prayon than in Ganges. The results suggest that Cd uptake by the low Cd‐accumulating ecotype (Prayon) may be mediated partly via Ca channels or transporters for Zn and Mn. By contrast, there may exist a highly selective Cd transport system in the root cell membranes of the high Cd‐accumulating ecotype (Ganges) of T. caerulescens.