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Spatial variability of soil total nitrogen in PopuLus tomentosa forestation land in south Hebei plain

机译:冀南平原毛白杨造林地土壤全氮的空间变异

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In order to investigate the spatial variability of soil total nitrogen (STN) contents in Populus tomentosa forestation land in South Hebei Plain, a gridding method was adopted for stationing and sampling in the 6.0 hm2 of P. tomentosa forestation land in South Hebei Plain in March. 2007. The land was divided into twenty four 50×50 m plots where soil samples were selected at varying soil layers: 0-20 cm, 20-40 cm and 40-60 cm. The results showed that the mean of STN contents above 60 cm soil layer was 0.40 g·kg-1 (from 0.05 to 0.82g·kg-1). Fertility level of the soil in the P. tomentosa forestation land in South Hebei Plain is classified as extremely-low level. The STN content generally had moderate spatial variability since the coefficient of variation (CV) at each layer was increased with the increase of soil depth. The horizontal variability of STN at 0-20 cm soil layer was that the value first increased and then declined from west to east and had a twice trend of first increase and then decrease from north to south. At 20-40 and 40-60 cm soil layers, the horizontal variability of STN content was: the value declined gradually from west to east. while rose up gradually from north to south. The STN content at the depth of 0-20 cm was obviously higher than the value at the depth of 20-40 cm and 40-60 cm (P<0.01). In conclusion. the thin soil layer, sandy texture and severe wind erosion and desertification are contributed to the relative lower STN in the P. tomentosa forestation land in South Hebei Plain, and the proper methods of irrigation and fertilization should be taken to improve the soil fertility.
机译:为了研究河北平原毛白杨造林地土壤总氮含量的空间变异性,采用网格化方法对河南平原毛白杨造林地3月份的6.0 hm2进行定位和采样。 。 2007年。该土地被分成二十四个50×50 m的地块,在这些样地中选择了0-20 cm,20-40 cm和40-60 cm不同土层的土壤样本。结果表明:60 cm土层以上STN平均含量为0.40 g·kg-1(0.05〜0.82g·kg-1)。河北南部平原毛竹林地土壤的肥力水平被列为极低水平。 STN含量通常具有中等的空间变异性,因为每层的变异系数(CV)随着土壤深度的增加而增加。 STN在0-20 cm土层的水平变化是,该值先从西向东升高,然后从西向东递减,并具有从北向南先升高然后从北递减的两倍趋势。在20-40和40-60 cm土层上,STN含量的水平变化为:该值从西向东逐渐减小。而从北到南逐渐上升。 0-20 cm深度的STN含量明显高于20-40 cm和40-60 cm深度的STN含量(P <0.01)。结论。薄薄的土壤层,沙质的质地,严重的风蚀和荒漠化是河北平原南部毛竹林地STN相对较低的原因,应采取适当的灌溉和施肥方法以提高土壤肥力。

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