摘要
用同位素示踪技术研究水稻对14CO32-的吸收和积累动态,及其在水稻田中的行为特性。结果表明:通过水稻根系和浸于水中的茎杆下部吸收的14CO32-离子会向上部组织输送并形成积累趋势;在上部组织中,叶和茎杆上部的14C比活度随时间呈逐渐上升的趋势,而穗中的比活度于14d达最大值(271.9Bq/g)后又呈下降趋势;茎杆下部由于直接浸于水中,表现出对14CO32-离子的快速吸收、吸附,此后随时间呈下降趋势,根部表现出上升过程迟后于茎杆下部,其14C比活度也低于茎杆下部。上部组织(穗、叶和茎杆上部)中14C的百分含量随时间上升,而下部组织(茎杆下部和根)则相反,至试验后期(21~35d),其百分含量基本持平(约各占50%),14C从下部组织向上部组织输送的特征非常明显。
Dynamics of absorption and accumulation of ^14CO3^2- in rice were studied by isotope-tracer technology in order to study the behavior of ^14CO3^2- in rice paddy. The results showed that: ^14CO3^2- ions absorbed by roots and lower part of stems (LPS) in water were transferred to upper part of rice plant(UPR), and presented a tendency of accumulation. In UPR, the specific activity of ^14 C in leaves and upper part of stems (UPS) slowly increased with time while it in tassels tended to decrease after reaching the maximum (271.9Bq/g) at the 14th day. ^14CO3^2- ions were absorbed quickly in LPS dipping in water, and then slowly declined. Compared with LPS, the increasing tendency in roots was slowly and the specific activity of ^14C was also lower as roots embed in soil. The percentage of ^14C in UPR (tassels, leaves and UPS) was increscent with time, but reversed in LPR. During the late stage of experiment (21 ~35d), percentage in both UPR and LPR were almost equal, about 50% respectively. The characteristic of ^14C transferred from LPR to UPR was greatly evident.
出处
《核农学报》
CAS
CSCD
北大核心
2005年第5期375-378,共4页
Journal of Nuclear Agricultural Sciences
基金
国家自然科学基金(20477040)