2002Acta Pratacultural ScienceRequires access

Studies on the characteristics of soil fertility and relationshipamong nutritive factors in alpine grassland soil of Qilian mountains

Zhang De

Open publisher page 1 citations

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 subalpine shrub soil, alpine meadow soil, alpine chernozem and subalpine meadow soil. The organic matter content (OMC) in this group was above 14%. Group B included alpine chestnut soil, alpine brown soil, subalpine steppe soil and alpine steppe soil and their OMC were below 4%. Among 8 soil types, the subalpine 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 subalpine 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 subalpine grassland soil, nitrogen fertilizer or legume should be used at the same time.

About this research paper

What this paper is about

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 subalpine shrub soil, alpine meadow soil, alpine chernozem and subalpine meadow soil. The organic matter content (OMC) in this group was above 14%. Group B included alpine chestnut soil, alpine brown soil, subalpine steppe soil and alpine steppe soil and their OMC were below 4%. Among 8 soil types, the subalpine 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 subalpine 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 subalpine grassland soil, nitrogen fertilizer or legume should be used at the same time.

Why it matters

OpenAlex reports 1 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available 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 subalpine shrub soil, alpine meadow soil, alpine chernozem and subalpine meadow soil. The organic matter content (OMC) in this group was above 14%. Group B included alpine chestnut soil, alpine brown soil, subalpine steppe soil and alpine steppe soil and their OMC were below 4%. Among 8 soil types, the subalpine 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 subalpine 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 subalpine 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

Related papers

Back to paper searchBrowse research topicsOriginal source
Studies on the characteristics of soil fertility and relationshipamong nutritive factors in alpine grassland soil of Qilian mountains — Research Paper | ScholarLens