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Effect of conversion of sugarcane plantation to forest and pasture on soil carbon in Hawaii

机译:夏威夷州甘蔗人工林退牧对土壤碳的影响

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摘要

It is well known that land use change can affect soil C storage of terrestrial ecosystems either by altering the biotic processes involved in carbon cycling or by altering abiotic processes such as carbon adsorption on soil minerals. Relatively few studies, however, have examined the dynamics of soil C pools after conversion of farmland to forest or pasture. We selected three pairs of secondary forests and pastures that originated from the same abandoned sugarcane (interspecific hybrids of Saccharum spp.) land in the wet tropics of Hawaii to examine whether forest or pasture converted from farmland is more effective in sequestering C in soils. We compared the soil C pool, soil chemistry, and stable C isotope ratios between the forests and pastures. We found that total soil C was greater (P<0.01) in forests than in the pastures 22 years after land conversion. The percentages of SOC_4 in the pastures were significantly higher than in the secondary forests in both soil layers. The percentages of SOC_3 in the pastures were lower than in the secondary forests in both soil layers. The net SOC_3 increase in the forest soils at 0-10 and 10-25 cm was 28.6±5.6 and 43.9±3.2 Mg ha~(-1) while net SOC_4 increase in pasture soils at these respectiverndepths was 18.8 ±2.2 and 26.1 ±2.7 Mg ha~(-1). We found that the net increases of SOC_3 in both soil layers in the forest were greater (P<0.01) than the net increases of SOC_4 in the respective soil layers in the pasture. Aluminum saturation was greater (P<0.01) in the forests than the pastures in both soil layers. There was no difference in oxalate extractable Fe concentration between the forests and the pastures but oxalate extractable Al concentration in both soil layers was greater (P<0.05) in forests than the pastures. Our findings indicated that reforestation of abandoned sugarcane farmland in Hawaii is more effective in soil C increase and stabilization than conversion to pasture.
机译:众所周知,土地利用变化可以通过改变碳循环所涉及的生物过程或通过改变非生物过程(例如土壤矿物上的碳吸附)来影响陆地生态系统的碳储量。但是,相对较少的研究检查了农田转化为森林或牧场后土壤碳库的动态。我们选择了三对源自夏威夷湿热带地区相同废弃荒地(Saccharum spp。的种间杂种)土地的次生森林和牧场,以研究从农田转换而来的森林或牧场是否更有效地将C螯合到土壤中。我们比较了森林和牧场之间的土壤碳库,土壤化学性质和稳定的碳同位素比。我们发现,土地转化后22年,森林中的土壤总C大于牧场(P <0.01)。在两个土壤层中,牧场中SOC_4的百分比均显着高于次生林。在两个土壤层中,牧场中SOC_3的百分比均低于次生林。在0-10和10-25 cm处森林土壤的SOC_3净增加为28.6±5.6和43.9±3.2 Mg ha〜(-1),而在这三个深度下的牧场土壤中SOC_4的净增加为18.8±2.2和26.1±2.7镁ha〜(-1)。我们发现,森林中两个土壤层中SOC_3的净增加都比牧场中各个土壤层中SOC_4的净增加大(P <0.01)。在两个土壤层中,森林中的铝饱和度均大于牧场(P <0.01)。森林和牧场之间草酸盐可提取的Fe浓度没有差异,但森林中两个土壤层中草酸盐可提取的Al的浓度均高于牧场(P <0.05)。我们的发现表明,夏威夷废弃的甘蔗农田的重新造林在土壤碳的增加和稳定方面比转化为牧场更有效。

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