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The relation of surface environmental factor to depth of groundwater on Horqin sandy land in Tong Liao city, China

机译:通辽市科尔沁沙地地表环境因子与地下水深度的关系

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This paper reports the relationship between surface environmental factors and depth of groundwater on Horqin sandy land in Tongliao dry, China. The main findings are: 1) The plants in Horqin area are divided into three basic kinds (1) The plant typewhich is not affected directly by groundwater in drifting sand dunes, and the fixation and semi-fixation sand dunes, (2) The transitional plant type which exists in transitional zone between sand dunes and lower ground for pasture, and (3) The plant type affected by groundwater. which exists in bog hole and lower ground ranked between sand dunes and lower ground for pasture. 2) Groundwater table in Horqin sandy land shows a cyclic variation due to hydro-meteorological element. The lowering of the groundwater table is accelerated by the prevalent speed of wind erosion and desertification arid frequency of sandstorm. 3) Thickness of annual rings of tree showed a significant positive correlation with the amount of precipitation and their correlation coefficient increases wirh rhe depth of groundwarer. When rhe depth of groundwater reaches 6m or so, the growth of the kind of tree used in an experiment depends on the amount of precipitation in general. 4) The average thickness of annual rings of a tree for years has a negative exponential correlation with the depth of groundwater. 5) The wind erosion depth increases with the depth of groundwarer. and desertification is accelerated through excessive production activity by human beings.
机译:本文报道了通辽干旱地区科尔沁沙地的地表环境因子与地下水深度的关系。主要发现有:1)科尔沁地区的植物分为三种基本类型:(1)不受沙丘中的地下水直接影响的植物类型,以及固定和半固定沙丘的植物;(2)过渡性植物。在沙丘和牧场低地之间的过渡带中存在的植物类型;(3)受地下水影响的植物类型。它存在于沼泽洞和低地之间,位于沙丘和草场之间。 2)科尔沁沙地地下水位因水文气象要素而表现出周期性变化。普遍的风蚀和沙漠化以及沙尘暴的频率加快了地下水位的下降。 3)树木年轮的厚度与降水量呈显着的正相关,并且它们的相关系数随着地埋深度的增加而增加。当地下水的流变深度达到6m左右时,实验中所用树种的生长通常取决于降水量。 4)数年的树木年轮平均厚度与地下水深度呈负指数相关。 5)风蚀深度随地埋深度的增加而增加。人类过度的生产活动加剧了荒漠化。

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