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  • Taggard, Kenneth L.  (2)
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  • 1
    In: Agronomy Journal, Wiley, Vol. 71, No. 4 ( 1979-07), p. 523-528
    Kurzfassung: The biological yield potential of winter annual range legumes is influenced by the timing of rainfall adequate to ensure germination. If rains are late, the establishment phase of growth must occur at cold soil and air temperatures. On low‐P soils, this combination of abiotic factor constraints can limit symbiotic N fixation. We conducted three controlled‐environment experiments to compare the seedling growth of rose clover ( Trifolium hirtum All., ‘Hykon’) and subterranean clover ( T subterrateum L., ‘Mt. Barker’, hereafter referred to as subclover) on a P‐deficient soil (Sobrante‐Las Posas association), simulating winter conditions of cold soils and low light. Comparative growth responses, especially intraplant dry matter partitioning and nodulation, were observed for several soil P availability levels. A sunlit phytotron provided a common shoot environment of seasonal (fall/winter) ambient light intensity and photoperiod, with a programmed smooth diurnal temperature cycle of 20 C maximum and 5 C minimum. Three independently‐controlled water baths maintained soil temperature experiments at a constant 5 C, a constant 10 C, and a diurnal 5 C to 10 C alternation. Phosphorus levels were 0, 45, 90, and 180 kg/ha equivalents. Growth intervals (5 ± 0.5 trifoliolate‐leaf stage), varied between 58 and 114 days. Leaf area of subclover was greater than that of rose clover, and responded more to increasing P levels. Leaf areas tended to increase with higher soil temperatures. Nodule weight was positively correlated with leaf area; nodule weight:leaf area regressions suggested that nodule development was adequate at 5 C and that nodule development was primarily related to time rather than to morphological development of the shoot. Nodule weights were similar for the two species, and low at 0 P. The results suggest that while the practical soil threshold temperature for overall growth is near 5 C, some intraplant growth processes may proceed, but only at adequate, availability levels of mineral nutrients. These relationships may be particularly important where range annual legumes are being introduced as part of a more general range improvement program.
    Materialart: Online-Ressource
    ISSN: 0002-1962 , 1435-0645
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 1979
    ZDB Id: 1471598-3
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Online-Ressource
    Online-Ressource
    Wiley ; 1989
    In:  Crop Science Vol. 29, No. 3 ( 1989-05), p. 758-763
    In: Crop Science, Wiley, Vol. 29, No. 3 ( 1989-05), p. 758-763
    Kurzfassung: Considerable variation exists in recommendations for the use of N during establishment of forage legumes. Abundant literature documents the inhibition of N 2 fixation by applied N, but few experiments determined the consequences of its subsequent removal. In this study the effects of NH 4 NO 3 on the growth and N 2 fixation of subterranean clover ( Trifolium subterraneum L.) were investigated. Plants were grown in a greenhouse from seed with a modified Hoagland's solution containing 0, 2, 4, 6, 8, and 12 m M NH 4 NO 3 for 80 d. The plants were then divided into two groups, the N treatments continued for one (+ N) group and the other group given an N‐free Hoagland's solution (−N) for an additional 21 d. Total dry wt. (DM), apparent N 2 fixation (ANF), leaf area (LA), and shoot N concentration were measured and levels of photosynthetically active radiation (PAR) were monitored continuously during daylight hours. Per plant DM accumulation increased exponentially over 101 d. Neither DM nor LA accumulation was influenced by NH 4 NO 3 at 50 and 80 d. At 101 d, both DM and LA were greater ( P 〈 0.01) for the 2 m M treatment than for the control, and each declined linearly ( P 〈 0.01 for ± NPM and −NLA; P 〈 0.05 for +NLA) with increasing NH 4 NO 3 levels. Differences in slopes were not significant (P 〉 0.05). Leaf area ratio (LAR) was not influenced by NH 4 NO 3 treatments at any of the sampling dates. Nitrogen per plant was greater than the control (P 〈 0.01) for both ± N at 2 m M , and it declined linearly ( P 〈 0.05 for +N; P 〈 0.01 for −N) with increasing NH 4 NO 3 levels. A reduction in per‐plant ANF was significant ( P 〈 0.01) over all NH 4 NO 3 levels at 50 and 101 d and over 6 to 12 m M levels at 80 d. Plants previously grown at 6 to 12 m M levels (−N) recovered much of their ANF ability at 101 d, while ANF for + N plants declined (P 〈 0.01) across all N levels. Expression of ANF on a per unit DM or LA basis improved interpretation of these data. Nitrogen concentration of shoots for all treatments except 12 m M −N was similar to the control at 101 d. Overall, N yields per plant were best explained by DM accumulation from 80 to 101 d. The ability to rapidly recover N 2 ‐fixing ability following depletion of inorganic soil solution N provides opportunity for early season use of N fertilizer in annual range systems.
    Materialart: Online-Ressource
    ISSN: 0011-183X , 1435-0653
    Sprache: Englisch
    Verlag: Wiley
    Publikationsdatum: 1989
    ZDB Id: 1480918-7
    Standort Signatur Einschränkungen Verfügbarkeit
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