Welcome to Acta Prataculturae Sinica ! Today is Share:

Acta Prataculturae Sinica ›› 2022, Vol. 31 ›› Issue (2): 14-24.DOI: 10.11686/cyxb2020563

Previous Articles     Next Articles

Effects of biochar addition on nutrient levels and humus and its components in dry farmland soils on the Loess Plateau

Zhan-dong PAN1,2(), Qian-qian MA1,2, Xiao-long CHEN1,2, Li-qun CAI1,2(), Xue-mei CAI1,2, Bo DONG1,3, Jun WU1,2, Ren-zhi ZHANG1,2   

  1. 1.College of Resources and Environmental Sciences,Gansu Agricultural University,Lanzhou 730070,China
    2.Gansu Provincial Key Laboratory of Arid Land Crop Science,Gansu Agricultural University,Lanzhou 730070,China
    3.Gansu New Fertilizer Creation Engineering Laboratory,Institute of Soil Fertilizer,and Water-saving Agriculture,Gansu Academy of Agricultural Sciences,Lanzhou 730070,China
  • Received:2020-12-15 Revised:2021-03-10 Online:2022-02-20 Published:2021-12-22
  • Contact: Li-qun CAI

Abstract:

Severe soil erosion in the Loess Plateau leads to a significant decrease in some soil nutrients and quality. Biochar can increase crop yield and soil biological activity, so it is widely used in soil improvement. However, it is not clear whether biomass charcoal can improve the physical and chemical properties of loessial soil by improving soil nutrient levels, and humus composition and content. This study investigates this question for a loessial soil on the Loess Plateau. The research was conducted at the Dry Farming Experiment Station of Gansu Agricultural University. A four-year field trial was set up with six biomass charcoal addition levels (0, 10, 20, 30, 40, 50 t·ha-1) to determine the changes in soil nutrient levels, organic carbon components, combined humus composition and composition. It was found that addition of biochar at a rate of 20 t·ha-1 or above significantly increased the soil heavy fraction organic carbon (HFOC), light fraction organic carbon (LFOC), organic matter and total nitrogen contents. Biochar addition had no significant effect on soil total phosphorus or potassium levels, but addition of biochar at 10 t·ha-1 significantly increased soil available phosphorus and decreased available potassium. This effect was progressively reversed as the rate of biochar increased and the addition of biochar at 60 t·ha-1 significantly increased the available potassium content but tended to reduce the available phosphorus content. When biochar was added at 20 t·ha-1 and above, the content of soil loose combined humus (LCH) was increased by 47.50%-65.83% (P<0.05); When biochar was added at rates in excess of 30 t·ha-1, the content of humus constituent fulvic acid (FA) was increased by 78.79%-133.33% (P<0.05). LFOC, HFOC and LCH were the components that contributed most to the increase of soil total organic carbon following biochar addition. Among these the interpretation rate of LFOC and HFOC to TOC were 72.55% and 89.74% respectively. This research provides increased understanding of the soil chemistry changes after addition of biomass charcoal in soil improvement and fertility improvement in dry farming areas of the Loess Plateau.

Key words: biochar, Loess Plateau, soil nutrient, organic carbon fractions, humic substance