USE OF ICP-MS AND B-10 TO TRACE THE MOVEMENT OF BORON IN PLANTS AND SOIL

被引:21
作者
BROWN, PH [1 ]
PICCHIONI, G [1 ]
JENKIN, M [1 ]
MU, HN [1 ]
机构
[1] UNIV ADELAIDE,WAITE AGR RES INST,DEPT PLANT SCI,GLEN OSMOND,SA 5064,AUSTRALIA
关键词
D O I
10.1080/00103629209368773
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Of all the plant essential elements, boron (B) is the least understood. This lack of understanding is due in part to the unavailability of a suitable isotope to trace the movement of B. With the introduction of the inductively coupled plasma mass spectrometry (ICP-MS) in the mid 1980s, it is now possible to utilize the stable isotope B-10 as a tracer of B. The low detection limits of the ICP-MS also allow determination of B concentrations in small samples such as membrane or cell wail preparations. In this paper, we describe the use of enriched B-11 and B-10 to trace B uptake in intact plants (soil and nutrient solution application), isolated protoplasts, leaf and stem tissue (foliar application). Results suggest that stable isotope labelling is an effective and inexpensive method of monitoring B movement in plants and soil. The recovery of enriched B in fruit and nut tissue suggests B may be at least partially phloem mobile. Enriched B isotopes were effectively used to monitor B uptake into isolated protoplasts and whole plants. Monitoring soil B movement was also accomplished using this procedure. Differences in the natural abundance of B isotopes (B-10:B-11 ratio) at different locations and in different soil types is discussed. Description of ICP-MS instrumental parameters, digestion techniques, isotopic enrichment and ratioing parameters is included.
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页码:2781 / 2807
页数:27
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