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Litterfall, nutrient return, and leaf-litter decomposition in four plantations compared with a natural forest in subtropical China

机译:与亚热带天然林相比,四种人工林的凋落物,养分返回和叶片凋落物分解

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摘要

The amount and pattern of litterfall, its nutrient return, initial chemistry of leaf litter, and dynamics of N, P and K associated with leaf-litter decomposition were studied in 33-year-old plantations of two coniferous trees, Chinese fir (Cunninghamia lanceolata, CF) and Fokienia hodginsii (FH), and two broadleaved trees, Ormosia xylocarpa (OX) and Castanopsis kawakamii (CK), and compared with that of an adjacent natural forest of Castanopsis kawakamii (NF, similar to150 year old) in Sanming, Fujian, China. Mean annual total litterfall over 3 years of observations was 5.47 Mg.ha(-1) in the CF, 7.29 Mg.ha(-1) in the FH, 5.69 Mg.ha(-1) in the OX, 9.54 Mg.ha(-1) in the CK and 11.01 Mg.ha(-1) in the NF respectively; of this litterfall, leaf contribution ranged from 58% to 72%. Litterfall in the OX, CK, and NF showed an unimodal distribution pattern, while for the CF and FH, the litterfall pattern was multi-peak. The highest annual Ca and Mg returns were noticed in the FH and in the CK, respectively. The amounts of N, P, and K which potentially returned to the soil were the highest in the NF. The loss of dry matter in leaf litter exhibited a negative exponential pattern during the 750-day decomposition. Using the model x(t) = A + Be-kt, the annual dry matter decay constants (k) ranged from 1.157 in CF to 4.619 in OX. Initial lignin concentration and lignin/N ratios showed significantly negative correlations with k (r = -0.916, P = 0.011; r = -0.473, P = 0.041), whereas initial N concentration showed low positive correlations (r = 0.225, P = 0.038). Using the model x(t) = A + Be-kt, the decay constant of N (k(N)) ranged from 0.769 in CF to 4.978 in OX; the decay constant of P (k(p)) ranged from 1.967 in the OX to 4.664 in the NF; and the decay constant of K (k(K)) seemed very similar among these forests (5.250-5.992). The decay constants of nutrients during leaf-litter decomposition can be arranged in the sequence of k(K) > k(P) > k(N), except for leaf litter of OX where k(K) > k(N) > k(P).
机译:研究了两棵针叶树(杉木(Cunninghamia lanceolata))的33年龄人工林的凋落物的数量和模式,其养分归还,叶片凋落物的初始化学以及与凋落物分解相关的N,P和K的动态。 (CF)和Fokienia hodginsii(FH),以及两棵阔叶乔木(Ormosia xylocarpa(OX)和Castanopsis kawakamii(CK)),并与三明的Castanopsis kawakamii(NF,类似于150岁)的相邻天然林相比,中国福建。在3年的观测中,CF的年平均凋落物总量为CF中的5.47 Mg.ha(-1),FH中的7.29 Mg.ha(-1),OX的5.69 Mg.ha(-1),9.54 Mg.ha (-1)在CK中和11.01 Mg.ha(-1)在NF中;在这些凋落物中,叶子的贡献从58%到72%不等。 OX,CK和NF的凋落物呈单峰分布,而CF和FH的凋落物呈多峰。在FH和CK中分别注意到最高的年度Ca和Mg回报。可能返回土壤的氮,磷和钾的含量在NF中最高。在750天的分解过程中,枯枝落叶中干物质的流失呈负指数模式。使用模型x(t)= A + Be-kt,年干物质衰减常数(k)范围从CF中的1.157到OX中的4.619。初始木质素浓度和木质素/氮比与k呈显着负相关(r = -0.916,P = 0.011; r = -0.473,P = 0.041),而初始N浓度呈低正相关(r = 0.225,P = 0.038) )。使用模型x(t)= A + Be-kt,N(k(N))的衰减常数在CF的0.769到OX的4.978之间; P(k(p))的衰减常数从OX的1.967到NF的4.664。这些森林中K的衰减常数(k(K))看起来非常相似(5.250-5.992)。叶子凋落物分解过程中养分的衰减常数可以按k(K)> k(P)> k(N)的顺序排列,但OX的凋落物除外,其中k(K)> k(N)> k (P)。

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