Neill Christopher, Piccolo Marisa C, Cerri Carlos C, Steudler Paul A, Melillo Jerry M, Brito Marciano
The Ecosystems Center, Marine Biological Laboratory, Woods Hole, MA 02543. USA fax: 508 457 1548; e-mail:
Centro de Energia Nuclear na Agricultura (CENA), Universidade de São Paulo, Avenida Centenário 303, Caixa Postal 96, CEP 13416000, Piracicaba, SP, Brazil, , , , , , BR.
Oecologia. 1997 Apr;110(2):243-252. doi: 10.1007/s004420050157.
Previous studies of the effect of tropical forest conversion to cattle pasture on soil N dynamics showed that rates of net N mineralization and net nitrification were lower in pastures compared with the original forest. In this study, we sought to determine the generality of these patterns by examining soil inorganic N concentrations, net mineralization and nitrification rates in 6 forests and 11 pastures 3 years old or older on ultisols and oxisols that encompassed a wide variety of soil textures and spanned a 700-km geographical range in the southwestern Brazilian Amazon Basin state of Rondônia. We sampled each site during October-November and April-May. Forest soils had higher extractable NO-N and total inorganic N concentrations than pasture soils, but substantial NO-N occurred in both forest and pasture soils. Rates of net N mineralization and net nitrification were higher in forest soils. Greater concentrations of soil organic matter in finer textured soils were associated with greater rates of net N mineralization and net nitrification, but this relationship was true only under native forest vegetation; rates were uniformly low in pastures, regardless of soil type or texture. Net N mineralization and net nitrification rates per unit of total soil organic matter showed no pattern across the different forest sites, suggesting that controls of net N mineralization may be broadly similar across a wide range of soil types. Similar reductions in rates of net N transformations in pastures 3 years old or older across a range of textures on these soils suggest that changes to soil N cycling caused by deforestation for pasture may be Basin-wide in extent. Lower net N mineralization and net nitrification rates in established pastures suggest that annual N losses from largely deforested landscapes may be lower than losses from the original forest. Total ecosystem N losses since deforestation are likely to depend on the balance between lower N loss rates from established pastures and the magnitude and duration of N losses that occur in the years immediately following forest clearing.
先前关于热带森林转变为牧场对土壤氮动态影响的研究表明,与原始森林相比,牧场的净氮矿化率和净硝化率较低。在本研究中,我们试图通过检测巴西亚马孙盆地西南部朗多尼亚州多种土壤质地、跨度700公里地理范围内的6片森林和11片树龄3年及以上的牧场土壤中的无机氮浓度、净矿化率和硝化率,来确定这些模式的普遍性。我们在10月至11月以及4月至5月对每个地点进行了采样。森林土壤中可提取的硝态氮和总无机氮浓度高于牧场土壤,但森林和牧场土壤中都存在大量硝态氮。森林土壤中的净氮矿化率和净硝化率较高。质地较细的土壤中较高的土壤有机质浓度与较高的净氮矿化率和净硝化率相关,但这种关系仅在原生森林植被下成立;牧场中的速率普遍较低,与土壤类型或质地无关。每单位土壤总有机质的净氮矿化率和净硝化率在不同森林地点没有呈现出特定模式,这表明在广泛的土壤类型中,净氮矿化的控制因素可能大致相似。在这些土壤上,不同质地的3年及以上牧场中净氮转化速率都有类似程度的降低,这表明因毁林改牧场导致的土壤氮循环变化可能在整个流域范围内存在。已建成牧场中较低的净氮矿化率和净硝化率表明,大面积毁林后的景观每年的氮损失可能低于原始森林的损失。自毁林以来生态系统的总氮损失可能取决于已建成牧场较低的氮损失率与森林砍伐后立即出现的氮损失量及持续时间之间的平衡。