Rehder H
Institut für Botanik und Mikrobiologie der Technischen Universität München, Germany.
Oecologia. 1976 Dec;22(4):411-423. doi: 10.1007/BF00345317.
Four plots of alpine meadow communities (mats) of the Northern Calcareous Alps are compared with regard to dry substance (DS), N-, P-, and K-content of living and dead overground and total underground phytomass. The Caricetum firmae F (altitude 2,010 m) produces the least green mass but accumulates the highest amount of dead substance (litter). In all parts it has the lowest content of N, P, K. The opposite is the Caricetum ferrugineae C (1,900 m): Small dead mass, but high production of green mass and high content of N and K in the living overground and total underground phytomass. The Nardetum N (1,930 m) is marked by relatively high amounts of P in living and dead parts. The Seslerio-Semperviretum S (2,150 m) is intermediate but with rather low contents of K.In each plot the average total nitrogen found in the underground phytomass is about 200% of the amount found in the living overground phytomass. This suggests a similar relation of living mass in the two components of the total phytomass.The fluctuations in the phytomass throughout the growing season are represented for S. The green mass increase is about 200g DS with about 3 g N/m. This amount corresponds to the average mineralization supply of N during the growing season as obtained by the field incubation method (3.3 g/m, in 0-15 cm depth of the soil). In C the average mineralization is lower whereas the green mass production amounts to 300 g DS/m with 5.5 g N/m. This discrepancy supports again our hypothesis of an "internal nitrogen cycle" in the Carex ferruginea community. In F and N we find a lower incorporation of N into the annual green mass production compared with the N mineralized in the upper soil layers (Table 1).Lactate-soluble P and K were as a rule not accumulated in our soil incubation tests. The actual values and their amplitude during the growing season scarcely coincide with the differences of P and K in the green mass.
对北钙质阿尔卑斯山的四块高山草甸群落(草垫)进行了比较,分析了地上和地下活体及死亡植物总生物量的干物质(DS)、氮、磷和钾含量。坚挺苔草群落F(海拔2010米)产生的绿色生物量最少,但积累的死亡物质(凋落物)最多。在各个部分,其氮、磷、钾含量最低。相反,铁锈苔草群落C(1900米):死亡生物量少,但绿色生物量产量高,地上活体和地下植物总生物量中的氮和钾含量高。高山火绒草群落N(1930米)的特点是活体和死亡部分的磷含量相对较高。刺柏-长生草群落S(2150米)处于中间水平,但钾含量相当低。在每个样地中,地下植物生物量中发现的平均总氮量约为地上活体植物生物量中氮量的200%。这表明总植物生物量的两个组成部分中活体生物量的关系相似。展示了样地S整个生长季节植物生物量的波动情况。绿色生物量增加约200克DS,含氮约3克/平方米。这个量与通过田间培养法获得的生长季节氮的平均矿化供应量相对应(3.3克/平方米,土壤深度0 - 15厘米)。在样地C中,平均矿化量较低,而绿色生物量产量为300克DS/平方米,含氮5.5克/平方米。这种差异再次支持了我们关于铁锈苔草群落中“内部氮循环”的假设。与上层土壤层中矿化的氮相比,在样地F和N中,我们发现氮在年度绿色生物量生产中的掺入量较低(表1)。在我们的土壤培养试验中,乳酸可溶性磷和钾通常不会积累。生长季节的实际值及其变化幅度几乎与绿色生物量中磷和钾的差异不一致。