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Poplar plantations in coastal China: towards the identification of the best rotation age for optimal soil carbon sequestration

机译:中国沿海杨树人工林:确定最佳轮作年龄以优化土壤碳固存

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Poplar plantations are an important resource in China, which possess significant potential to offset carbon (C) emissions through the sequestration of atmospheric carbon dioxide (CO2) within biomass and soil. The traditional rotation age of poplar plantations is determined by maximizing the economic return from timber production. However, the optimal rotation age that results in the highest level of carbon sequestration within the soil remains unclear. In this study, we examined the total C, nitrogen (N) and microbial biomass (SMB) content of soils, as well as other properties in 0-10, 10-25 and 25-40 cm soil profiles along a 0- to 20-yr chronosequence in a coastal region of Eastern China. Soil C stocks were determined for 1 m soil profiles, and the stand biomass in poplar plantations of different ages was investigated. We found that C concentrations within soils increased with plantation age, primarily in the topsoil layers. The periodic annual increment of C in soils peaked between stand ages of from 6 to 10 yr (0.71 t/ha/yr) and then decreased considerably at 17.5 yr, while the mean annual increment of C in soils was the highest at 15 yr (0.573 t/ha/yr). Soil C accumulation (i.e. soil C sequestration) was positively correlated with poplar biomass, soil N and SMB, and negatively correlated with soil potassium (K), calcium (Ca), magnesium (Mg) and sodium (Na), but not with sulphur (S) or phosphorus (P). Our results suggest that a rotation age of 15 yr is optimal for the sequestration of atmospheric CO2 in poplar plantations in the coastal region of Eastern China. The C sequestration capacity of soil was primarily controlled by poplar biomass, soil N and SMB.
机译:杨树人工林是中国的重要资源,具有通过封存生物质和土壤中的大气二氧化碳(CO2)抵消碳(C)排放的巨大潜力。杨树人工林的传统轮伐年龄是通过最大化木材生产的经济回报来确定的。然而,尚不清楚导致土壤中碳固存水平最高的最佳旋转年龄。在这项研究中,我们检查了土壤的总C,氮(N)和微生物生物量(SMB)含量,以及0至20的0-10、10-25和25-40 cm土壤剖面中的其他特性中国东部沿海地区的yr年代序列。确定了1 m土壤剖面的土壤碳库,并调查了不同年龄的杨树人工林的林分生物量。我们发现土壤中碳的浓度随种植年限的增加而增加,主要是在表土层。土壤中碳的周期性年增量在6至10年(0.71 t / ha / yr)的林龄之间达到峰值,然后在17.5年时显着下降,而土壤的C平均年增量在15年时最高( 0.573吨/公顷/年)。土壤碳积累(即固碳)与杨树生物量,土壤氮和SMB呈正相关,与土壤钾(K),钙(Ca),镁(Mg)和钠(Na)呈负相关,而与硫无关(S)或磷(P)。我们的结果表明,轮转年龄为15年最适合隔离华东沿海地区杨树人工林中的大气CO2。土壤的固碳能力主要受杨树生物量,土壤氮和中小颗粒的控制。

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