• 中文核心期刊
  • CSCD来源期刊
  • 中国科技核心期刊
  • CA、CABI、ZR收录期刊

砒砂岩与沙复配土养分含量及质地的垂直分布特征

Vertical Nutrient Distribution and Texture of Sandy Soil Added with Soft Rocks

  • 摘要:
      目的  研究不同比例砒砂岩添加对风沙土(沙)中碳氮比垂直分布规律的影响,为沙荒地改良以及复配土体地力的提升提供科学依据。
      方法  以位于陕西富平的砒砂岩与沙复配比小区为研究对象,选择砒砂岩与沙体积比分别为0:1(CK)、1:5(C1)、1:2(C2)和1:1(C3)的4个处理,分析复配土碳氮比(C/N)及其与土壤养分和质地的关系。
      结果  不同处理下土壤有机碳和全氮含量随着土层深度的增加而降低,有机碳平均值为1.45~2.70 g·kg-1且0~10 cm土层有机碳含量显著高于20~30 cm土层(P < 0.05);复配比单因素对有机碳产生显著影响,随着砒砂岩体积分数的增加,0~10 cm土层有机碳含量以C3处理最高。全氮平均值为0.28~1.31 g·kg-1,且0~10 cm土层全氮含量显著高于10~20 cm和20~30 cm土层,在0~10 cm土层中,C3处理的全氮含量显著高于其他处理,复配比和土层双因素对全氮均产生显著影响。C/N平均值为1.72~5.92,以0~10 cm最低,其值随着砒砂岩体积分数的增加而依次减小,以C3处理最为显著。硝态氮和铵态氮含量在各处理间的变化规律较为一致,平均值分别为33.56~197.00、5.51~70.02 mg·kg-1,以0~10 cm土层含量最高。砂粒含量随着土层的加深而逐渐增加,粉粒和黏粒则随着土层的加深而减少,随着砒砂岩体积分数的增加,土壤质地由砂土变为壤砂土再变为砂壤土。C/N与硝态氮和铵态氮均呈显著负相关关系,与土壤质地的颗粒组成也有一定的相关性,10~20 cm土层最为显著。
      结论  砒砂岩与沙复配比为1:1时可以促进0~10 cm表层土壤碳氮的积累,增强微生物的分解作用。

     

    Abstract:
      Objective  Effect of adding soft rocks to aeolian sandy soil in varied ratios on the vertical distributions of carbon (C), nitrogen (N), and texture of the soil was studied for improving fertility of the wasteland.
      Method  At Fuping, Shaanxi, soft rocks were blended to the local sandy soil in different ratios, i.e., 0:1 (CK), 1:5 (C1), 1:2 (C2), and 1:1 (C3) by volume to determine the C/N ratio and texture of soil in different depths.
      Result  The organic C and total N contents decreased with depth upon the additions. The average C content ranged from 1.45 g·kg-1 to 2.70 g·kg-1, and it was significantly higher in the 0-10 cm layer than 20-30 cm layer (P < 0.05). The mixing ratio had a significant effect on C, as the soft rocks increased (i.e., C3) so was C content in the top layer. The total N ranged 0.28-1.31 g·kg-1, and that in the 0-10 cm layer significantly higher than in the deeper soils. In the top layer, C3 rendered significantly more N than other treatments. The average C/N ranged 1.72-5.92 with the lowest in the 0-10 cm layer and a decline upon increased addition of soft rocks. The varied mixing ratios did not affect the nitrate N and ammonium N contents, which ranged 33.56-197.00 mg·kg-1 and 5.51-70.02 mg·kg-1, respectively, with the top layer being the highest. Sand content in the soil gradually increased with depth, while silt and clay particles decreased. Along with the addition of soft rocks the soil texture changed from sand to loamy sand, and to sandy loam. There was a significant inversed correlation between C/N and nitrate N and ammonium N, and a correlation with the particle size distribution in soil. The correlations were most significant in the 10-20 cm soil layer.
      Conclusion  The blending ratio of soft rocks and sand at 1:1 seemed to promote the C and N accumulation in the 0-10 cm layer of soil. It also enhanced the microbial degradation in the soil.

     

/

返回文章
返回