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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Evaluation of spatial and temporal changes of soil quality based on geostatistical analysis in the hill region of subtropical China
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Evaluation of spatial and temporal changes of soil quality based on geostatistical analysis in the hill region of subtropical China

机译:基于地统计学的亚热带丘陵区土壤质量时空变化评价

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摘要

Studies on the effect of land use alteration on the spatial variability of soil properties are limited. This study addressed the spatial and temporal variability of soil properties and changes of soil quality in a hill region of subtropical China using geostatistical methods. Soil samples from 0- to 15-cm depth were collected within 105 locations, on a 100 x 100 m grid basis over a 112-ha field, in 1985 and 1997, respectively. Soil properties showed large variability, with the highest coefficient of variation being observed for available P, the lowest for soil pH. Over the 12-year period, a significant decrease of soil organic matter appeared with original land use patterns of wasteland and paddy field, whereas other properties showed no significant changes. In addition to the alteration of wasteland, fertilization in upland increased available P and K, whereas the opposite appeared in forest restoration system. Changing wasteland into paddy field was found to increase soil fertility. A geostatistical analysis showed that all the soil properties (pH, organic mater, available P and K) and their changes between 1985 and 1997 were spatially structured. The nugget-to-sill ratio indicates a strong spatial dependence for soil pH, and a moderate spatial dependence for other properties. The ranges for soil properties in 1985 were equal to or larger than the diameter of the hills. Changing the land use patterns decreased the ranges for soil chemical properties. The ranges for soil pH and available K were similar to the radius of hills. Interpolation using kriging showed a spatial similarity among the soil properties. Soil properties decreased in the southeast quadrant of the research area where the land use was paddy field, while they increased around the center where arable upland was initially from wasteland. Thus, we propose a process to evaluate soil quality using the geostatistical methods as a potential analysis tool for monitoring changes at a farm scale.
机译:关于土地利用变化对土壤特性空间变异性影响的研究是有限的。本研究利用地统计学方法研究了亚热带丘陵地区土壤特性的时空变化和土壤质量的变化。分别在1985年和1997年在112公顷的土地上以100 x 100 m的网格在105个位置收集了0至15厘米深度的土壤样品。土壤特性显示出较大的变异性,有效磷的变异系数最高,土壤pH的变异系数最低。在过去的12年中,土壤有机质显着减少,其原始形式为荒地和水田,而其他性质则没有显着变化。除了改变荒地外,施肥还增加了山地的有效磷和钾,而在森林恢复系统中则相反。发现将荒地变成稻田可以增加土壤肥力。地统计分析表明,1985年至1997年之间的所有土壤特性(pH,有机质,有效磷和钾)及其变化都是空间结构的。块金/基石比表明对土壤pH的强烈空间依赖性,对其他性质的中等空间依赖性。 1985年的土壤特性范围等于或大于丘陵直径。改变土地利用方式减少了土壤化学性质的范围。土壤pH和有效钾的范围与丘陵半径相似。使用克里金插值法表明土壤属性之间存在空间相似性。在土地利用为稻田的研究区域的东南象限,土壤性质有所下降,而在耕地最初来自荒地的中心附近,土壤性质却有所增加。因此,我们提出了使用地统计方法作为评估农场规模变化的潜在分析工具来评估土壤质量的过程。

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