Studies on the characteristics of soil fertility and relationshipamong nutritive factors in alpine grassland soil of Qilian mountains
Zhang De
Abstract
Zhang De
Abstract
Abstrcat Studies in this paper showed that the nutrient factors varied very much among soil types in Qilian mountains and the studied 8 soil types could be grouped into two groups (Group A and B) according to nutritive factors. Group A included subalpine shrub soil, alpine meadow soil, alpine chernozem and subalpine meadow soil. The organic matter content (OMC) in this group was above 14%. Group B included alpine chestnut soil, alpine brown soil, subalpine steppe soil and alpine steppe soil and their OMC were below 4%. Among 8 soil types, the subalpine meadow soil had the highest OMC (19.61%) and alpine steppe soil had the lowest (1.77%). The pH value of 8 soil varied from 7.2 to 8.4. The variance trend of Cation Exchange Capacity (CEC) was similar with the OMC. The highest was subalpine meadow soil (65.61 m·e·/100g) and the lowest was alpine steppe (10.64 m·e·/100g). The characteristic of total nutrients was low phosphorus, high nitrogen and relative rich potash. However, the available nutrients were characterized with low available phosphorus. It was slightly higher in group A (between 13.2×10-6 and 28.2×10-6) and quite low in Group B (between 1.8×10-6 and 4.9×10-6). All nutritive factors had significant relationship each other except total potash, available potash and pH value. Especially the relationship coefficients of OMC and CEC with other factors were above 0.844. The nutritive condition suggests that phosphorus should be applied during grassland improvement and artificial grassland establishment. For alpine steppe soil and subalpine grassland soil, nitrogen fertilizer or legume should be used at the same time.
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Abstrcat Studies in this paper showed that the nutrient factors varied very much among soil types in Qilian mountains and the studied 8 soil types could be grouped into two groups (Group A and B) according to nutritive factors. Group A included subalpine shrub soil, alpine meadow soil, alpine chernozem and subalpine meadow soil. The organic matter content (OMC) in this group was above 14%. Group B included alpine chestnut soil, alpine brown soil, subalpine steppe soil and alpine steppe soil and their OMC were below 4%. Among 8 soil types, the subalpine meadow soil had the highest OMC (19.61%) and alpine steppe soil had the lowest (1.77%). The pH value of 8 soil varied from 7.2 to 8.4. The variance trend of Cation Exchange Capacity (CEC) was similar with the OMC. The highest was subalpine meadow soil (65.61 m·e·/100g) and the lowest was alpine steppe (10.64 m·e·/100g). The characteristic of total nutrients was low phosphorus, high nitrogen and relative rich potash. However, the available nutrients were characterized with low available phosphorus. It was slightly higher in group A (between 13.2×10-6 and 28.2×10-6) and quite low in Group B (between 1.8×10-6 and 4.9×10-6). All nutritive factors had significant relationship each other except total potash, available potash and pH value. Especially the relationship coefficients of OMC and CEC with other factors were above 0.844. The nutritive condition suggests that phosphorus should be applied during grassland improvement and artificial grassland establishment. For alpine steppe soil and subalpine grassland soil, nitrogen fertilizer or legume should be used at the same time.
Key concepts: Soil fertility, Potash, Agronomy, Steppe, Nutrient, Soil pH, Environmental science, Phosphorus