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Dynamics of Soil Organic Carbon Storage and Erosion due to Land Use Change (Illinois, USA)

机译:土地利用变化造成土壤有机碳储存与侵蚀的动态(伊利诺伊州,美国)

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Many factors including land use, management history, soil series, climate, and soil landscape processes affect the dynamics of soil organic carbon (SOC). The primary objective of this research was to determine the impact of land use change from timberland to cropland on erosion and the SOC storage on sloping landscapes of northwestern Illinois, USA. Typic Hapludalfs and Aquic Udifluvents were studied. The cropland area was previously cultivated from 1860 to 1929, between 1930 and 1979 the area was used for pastureland and was returned to cropland from 1980 to 2009. Since 1980, corn and soybean were grown on a yearly rotation system using a no-tillage system. The timberland area was never cleared and cultivated but was subjected to periodic grazing from 1860 to 2009. The SOC concentration of various soil layers, to a depth of 0.5 m, was measured and expressed on a volumetric basis. For both land uses, the subsurface layers had similar SOC levels. Results suggested that after 150 years the cropland landscape maintained or retained 69.4% of the total SOC of timberland on a volumetric basis. The other 30.6% of the SOC was either deposited in the water or released to atmosphere. This study only included SOC and did not attempt to address or include the amount of C stored in above ground timberland trees or cropland plants or in their root systems. Results suggest that if northwestern Illinois forest soils are cleared and used for cropland during the next 50 years, SOC will be retained in the sediment on lower landscape segments, released to atmosphere as CO2 or released to stream (water) in solution or attached to sediment. The initial timberland SOC levels will not be maintained when converted to cropland use even with a crop rotation which includes small grains and forages and no-till management systems for corn and soybean production. This land use conversion from timberland to cropland would result in greater SOC loss than if the area remained as forestland.
机译:许多因素包括土地利用,管理历史,土壤系列,气候和土壤景观过程影响土壤有机碳(SOC)的动态。本研究的主要目标是确定来自美国伊利诺伊州西北部倾斜景观的侵蚀土地利用变化对田间的影响。研究了典型的Hapludalfs和Aquic Udifflvents。此后,农田地区于1930年至1979年培养,1930年至1979年,该地区用于牧场,从1980年到2009年返回农田。自1980年以来,玉米和大豆在每年的旋转系统上种植了玉米和大豆。从未清除和培养,但是从1860年到2009年的周期性放牧。测量各种土壤层的SOC浓度,0.5μm的SOC浓度,并以体积的基础表达。对于这两种土地使用,地下层具有相似的SOC水平。结果表明,在150年后,农田景观在体内维持或保留了Timberland总SOC的69.4%。其他30.6%的SOC沉积在水中或释放到大气中。本研究仅包括SOC,并没有尝试解决或包括储存在地上的木材或农田植物的C的C的数量。结果表明,如果伊利诺伊州森林土壤被清除并在未来50年内用于农田,则SoC将保留在较低景观区段的沉积物中,释放到溶液中的大气或释放到溶液中或附着在沉积物中。即使在作物旋转中,在转换为耕地使用时,初始的Timberland SoC水平将不会被维持,这包括玉米和大豆生产的小谷物和饲料和无线管理系统。从Timberland到Cropland的这种土地使用转换将导致比该地区仍然作为林地的损失更大。

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