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RELA??O ENTRE SUCESS?O SECUNDáRIA, SOLO E SERAPILHEIRA EM UMA RESERVA BIOLóGICA NO ESTADO DO RIO DE JANEIRO, BRASIL

机译:巴西里约热内卢州生物保护区次生,土壤和小规模成功之间的关系

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The nutrient cycling is influenced by the successional stage. However, there are differences in the pattern of this dynamic. The present study aimed to evaluate the chemical attributes of the topsoil and litterfall in two abandoned plantations of the eucalyptus Corymbia citriodora in different stages of Atlantic Rainforest succession (YP: Young plantation; MP: mature plantation) at the Uni?o Biological Reserve, RJ. We tested the hypothesis that there is an increase in the nutrient contents in the topsoil and litterfall, the amount of litterfall and nutrient input to the soil, as the process of forest succession advances. We sampled the topsoil (depth of 0-10 cm; dry season/2008, rainy season/2008, dry season/2009, rainy season/2010) and litterfall (0.49 m 2 traps; 1.0 m above the forest floor; twice a month; 366 days) in five plots (5 m x 20 m) in the areas of PJ and PM. The topsoil in the PM area presented higher content of both total C and N, N + Al and Mn. On the other hand, the values of pH, C/N ratio and content of K, Fe and Zn were higher in the topsoil in the PJ area. No clear pattern was detected in terms of the P and Cu content in the topsoil. The annual litterfall was higher in the PM area, which presented higher content of total N and Mg, while higher C/N ratio and content of P and Ca occurred in the PJ area. We did not detected differences in terms of total C in litterfall. The input of C, N, P, K and Mg to the soil were higher by the litterfall in the area of PM, and there were no differences between PJ and MP in relation to the Ca input. We partly corroborated the tested hypothesis in relation to the nutrient content in topsoil, litter and nutrient input, although we completely corroborated the hypothesis in terms of litterfall.
机译:养分循环受演替阶段的影响。但是,这种动态模式存在差异。本研究旨在评估在Unijo生物保护区RJ大西洋雨林演替的不同阶段中,两个桉树Corymbia citriodora废弃林中表层土壤和凋落物的化学属性(YP:年轻人工林; MP:成熟人工林) 。我们检验了以下假设:随着森林演替的进行,表层土壤和凋落物中的养分含量,土壤中的凋落物和养分输入量都有增加。我们对表层土壤(深度为0-10厘米;旱季/ 2008,雨季/ 2008,旱季/ 2009,雨季/ 2010)和凋落物(0.49 m 2的圈套;森林地面以上1.0 m;每月两次)进行了采样; 366天)在PJ和PM地区的五个地块(5 mx 20 m)中。 PM区表层土壤中总C和N,N + Al和Mn含量较高。另一方面,PJ地区表层土壤的pH值,C / N比值以及K,Fe和Zn含量较高。就表层土壤中的P和Cu含量而言,没有检测到清晰的图案。 PM区域的年凋落物较高,表示总N和Mg含量较高,而PJ区域的C / N比以及P和Ca含量较高。我们没有发现凋落物总C的差异。由于凋落物在PM区域的沉降,向土壤中输入的C,N,P,K和Mg较高,并且相对于Ca输入,PJ和MP之间没有差异。尽管我们从凋落物方面完全证实了这一假设,但我们在一定程度上证实了与表土,凋落物和养分输入中的养分含量有关的检验假设。

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