首页> 外文期刊>Geoderma: An International Journal of Soil Science >Desertification effects on C and N content of sandy soils under grassland in Horqin, northern China.
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Desertification effects on C and N content of sandy soils under grassland in Horqin, northern China.

机译:沙漠化对科尔沁草原下沙质土壤碳氮含量的影响

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摘要

A field experiment was conducted in the Horqin sandy grassland, where desertification intensity gradients could be utilized to evaluate C and N concentration and storage in plants, litter and soil relative to the degree of desertification. The results showed that (1) grassland desertification could result in significant decreases in soil carbon and nitrogen storage, but the decrease of carbon and nitrogen concentration in plants and litter was not significant in the desertification processes; (2) carbon and nitrogen storage decreased significantly with increasing grassland desertification intensity; (3) carbon and nitrogen losses through desertification reached up to 107.53 Mt and 9.97 Mt in the Horqin Sand Land study plots during the last century, or 3.6 kg/m2 and 0.3 kg/m2; (4) 94.5% of carbon losses came from soil organic C, and 97.1% of the nitrogen lost by desertification came from soil total N; the carbon and nitrogen lost from plants and litter accounted for only 5.5% and 2.2% of total lost carbon and nitrogen, respectively; (5) most of the carbon and nitrogen are lost from the grassland in the early stages of the desertification process (in the light and moderate desertification stages), while C and N loss was less in later desertification stages; (6) the loss of soil organic C and N storage results mainly from the decrease of nutrient-rich soil fine particles eroded by wind. The decrease in plant and litter carbon and nitrogen storage results mainly from loss of soil potential productivity. Efforts to combat desertification in the Horqin Sand land should focus on preventing overgrazing and controlling soil erosion by wind in the critical early stages of the process.
机译:在科尔沁沙质草地上进行了野外试验,可以利用荒漠化强度梯度来评估相对于荒漠化程度的植物,凋落物和土壤中碳和氮的浓度和储量。结果表明:(1)草地荒漠化可导致土壤碳氮储量显着下降,但植物和凋落物中碳氮浓度的下降在荒漠化过程中并不显着; (2)草地荒漠化强度增加,碳,氮储量显着下降; (3)上个世纪在科尔沁沙地研究区通过荒漠化造成的碳和氮损失分别达到107.53 Mt和9.97 Mt,分别为3.6 kg / m2和0.3 kg / m2; (4)碳损失的94.5%来自土壤有机碳,荒漠化造成的氮损失97.1%来自土壤总氮。植物和凋落物的碳和氮损失分别仅占总碳和氮损失的5.5%和2.2%。 (5)在荒漠化早期(轻度和中度荒漠化阶段),大部分的碳和氮从草地上流失,而在沙漠化后期,碳和氮的损失较少; (6)土壤有机碳和氮储量的损失主要是由于风蚀侵蚀的富营养土壤细颗粒的减少。植物和凋落物碳氮存储量的减少主要是由于土壤潜在生产力的损失。科尔沁沙地的防治荒漠化工作应着眼于在该过程的关键早期阶段防止过度放牧和控制风对土壤的侵蚀。

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