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红壤剖面土壤养分对土地利用变化响应的敏感性

潘博1,段良霞1,张凤2,张亮1,袁红1,武乐乐1,盛浩1*   

  1. (1湖南农业大学资源环境学院, 长沙 410128;2湖南农业大学理学院, 长沙 410128)
  • 出版日期:2018-09-10 发布日期:2018-09-10

Responsive sensitivity of nutrients in red soil profile to land use change.

PAN Bo1, DUAN Liang-xia1, ZHANG Feng2, ZHANG Liang1, YUAN Hong1, WU Le-le1, SHENG Hao1*   

  1. (1College of Resources & Environment, Hunan Agricultural University, Changsha 410128, China; 2College of Science, Hunan Agricultural University, Changsha 410128, China).
  • Online:2018-09-10 Published:2018-09-10

摘要: 为了解红壤剖面土壤养分及其有效形态的分布以及对高强度土地利用的响应,本研究选取位于湘东大围山低丘陵地带同一景观单元内花岗岩红壤发育的4种毗邻的典型土地利用方式(包括樟树天然林以及由此转变而来的杉木人工林、板栗园和坡耕地),采用自制土钻以20 cm等间隔采集0~100 cm土壤样品,测定各土层的pH、有机质、大量元素(全氮、全磷、全钾)及其有效态(碱解氮、有效磷、速效钾)、中量(钙、镁)和微量元素(铁、锰、铜、锌)有效态的含量,并计算不同养分的敏感性指数(SI),分析土壤养分对土地利用变化响应的敏感性。结果表明,天然林地改为其他土地利用方式,0~100 cm土壤剖面有机质、全氮含量分别降低9%~55%和28%~57%,全磷含量则升高0.3~52倍,高强度的人类活动(如施肥)导致土壤剖面有机质和全氮的损失,但却引起磷素的累积。较之土壤全量养分(SI介于-0.6~1.5),有效态养分含量(SI介于-0.8~51.8)对土地利用变化的响应更为敏感。土壤有效磷(SI介于-0.8~51.8)、速效钾(SI介于-0.5~2.9)、有效态铁(SI介于-0.6~3.1)、有效态铜(SI介于-0.8~2.2)含量对土地利用变化以正响应为主,反映土地利用方式的转变提高了土壤剖面上养分的有效性。与表土相比,花岗岩红壤底土有效态养分(如碱解氮、有效磷、速效钾、有效态锰、锌)含量对土地利用变化的响应更敏感。不能简单地将不同土地利用方式浅层表土养分的研究结论外推到深层底土,应重视土地利用变化引起的底土养分(尤其是有效态和中、微量元素)的演变趋势。

关键词: 拟步甲, 鞘翅目, 阿拉善高原, 气象因子, 空间分布格局

Abstract: To understand the distribution of nutrients in soil profile and their responses to dramatic land use change, four adjacent land use systems, including natural forest, the resultantly converted Chinese fir plantation, Chinese chestnut orchard, and sloping cropland, were chosen. Those ecosystems were located at an identical landscape unit in the hilly region of Daweishan Mount, northeast Hunan Province. Soil samples of 0-100 cm were collected by soil auger with a 20 cm interval. The pH, soil organic matter, total and available macro-elements (total N, P, and K, and alkali-hydrolysable N, available P and K), medium elements (exchangeable Ca, Mg), and micronutrients (available Fe, Mn, Cu, and Zn) in each soil layer were analyzed. The sensitivity of soil nutrients in response to land use change was evaluated using the sensitivity index (SI). Results showed that the contents of soil organic matter and total N at 0-100 cm depth were reduced by 9%-55% and 28%-57%, respectively, while that of total P was increased by 0.3-52 folds following the conversion of natural forest to other land use types, indicating that dramatic human activities (such as fertilization) led to losses of soil organic matter and total N but an accumulation of P in soil profile. Compared with the soil total nutrient contents (with SI ranging from -0.6 to 1.5), available nutrient contents (SI: -0.8 to 51.8) were more sensitive to land use changes. The available P (SI: -0.8 to 51.8), K (SI: -0.5 to 2.9), Fe (SI: -0.6 to 3.1), and Cu (SI: -0.8 to 2.2) mainly presented positive responses to land use changes, indicating the enhanced availability of those nutrients in soil by land use change. The SI of available nutrients, including alkali-hydrolysable N, available P, K, Mn and Zn, in subsoil was generally higher than that in topsoil, implying that results focusing on the topsoil nutrients under various land use types cannot be simply extrapolated to the subsoil. Changes in subsoil nutrients (especially for available nutrients, medium nutrients, and micronutrients) caused by land use change should be received more attention.

Key words: Tenebrionidae, Alxa Plateau, meteorological factor, spatial distribution pattern, Coleoptera