首页> 外文会议>International Peat Congress; 20040606-11; Tampere(FI) >NUTRIENT CONCENTRATIONS IN PEAT - NEEDLE RELATIONS AND FROST HARDINESS IN SCOTS PINE IN VARIOUS CLIMATES IN NORTHERN CENTRAL FINLAND
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NUTRIENT CONCENTRATIONS IN PEAT - NEEDLE RELATIONS AND FROST HARDINESS IN SCOTS PINE IN VARIOUS CLIMATES IN NORTHERN CENTRAL FINLAND

机译:中部北部各种气候下旱生松树豆针养分含量和冻害的养分含量。

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We studied the soil and foliar nutritional characteristics of 145 tree stands on drained mires in northern central Finland (64°N-66°N). The peat and needle samples were collected from 145 sites. The frost hardiness of Scots pine needles was tested from three stands. Humification of the peat in the depth of 5 to 10 cm increased from H 3.6 to H 4.6 and mean nitrogen concentration from 1.6 % to 2.3 % respectively with the increasing temperature sum. Soil phosphorus and iron concentrations also increased from north to south. The results suggest that in the warmer climates the peat is more decomposed and provides sufficient amounts nitrogen for tree growth through natural mineralization. The needles were nitrogen deficient (N < 1.30 %) in coldest climates. The mean phosphorus concentration in the needles was over the deficiency limit (1.39 mg g~(-1)) in coldest climatic region and decreased in the warmer climates. The mean potassium concentration in the needles decreased from 4.6 mg g~(-1) to 3.8 mg g~(-1) as the temperature sum increased from 850 dd to 1050 dd. In September the needles were most cold hardened in the 850 dd climate, compared to those of the warmer regions. In October, however, there were only minor differences in the frost hardiness of the needles in different climates. The decrease in the frost hardiness along a temperature gradient in September was attributed to the well-known temperature control of frost hardiness. Frost hardiness in nitrogen rich sites, needles having the highest foliar nitrogen concentrations, were slightly lowered in the two warmest climates where as no effect was found in the coldest climate.
机译:我们研究了芬兰中北部(64°N-66°N)排水沟上的145个树桩的土壤和叶面营养特征。从145个地点收集了泥炭和针状样品。从三个立场测试了苏格兰松针的抗冻性。随着温度总和的增加,5到10 cm深度的泥炭湿度从H 3.6增加到H 4.6,平均氮浓度从1.6%增加到2.3%。从北到南,土壤中的磷和铁含量也有所增加。结果表明,在温暖的气候下,泥炭更易分解,并通过自然矿化为树木生长提供了足够的氮。在最冷的气候下,针头缺氮(N <1.30%)。在最冷的气候区域,针叶中的平均磷浓度超过了缺乏极限(1.39 mg g〜(-1)),而在较温暖的气候区域中则降低了。随着温度总和从850 dd增加到1050 dd,针中的平均钾浓度从4.6 mg g〜(-1)降低到3.8 mg g〜(-1)。与温暖地区相比,9月份在850 dd气候中,针最冷硬化。然而,在十月份,在不同气候下,针的耐霜冻性只有很小的差异。沿着温度梯度,9月霜冻强度降低是由于众所周知的霜冻温度控制。在两个最温暖的气候中,富含氮的部位(叶面氮浓度最高的针)的抗冻性略有降低,而在最冷的气候中则没有影响。

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