荒漠草原不同植物群落土壤氮矿化对水分梯度的响应
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国家自然科学基金项目(32260348);宁夏高等学校一流学科建设项目(NXYLXK2017A01)


Response of soil nitrogen mineralization of different plant communities in desert grassland to different moisture gradients
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The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan)

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    摘要:

    为探究宁夏东部荒漠草原常见植物群落土壤氮矿化对土壤干旱响应特征,选取5种植物群落,即蒙古冰草(Agropyron mongolicum),猪毛蒿(Artemisia scoparia),苜蓿(Medicago sativa),柠条(Caragana korshinskii)和黑沙蒿(Artemisia ordosica)作为研究对象,开展常见植物群落土壤氮矿化对水分干旱梯度(自然、饱和、干旱)的响应特征研究。结果表明:各植物群落0-20cm土壤水分均处于3.19%-5.17%范围,而0-200cm土壤平均含水量均具明显的垂直动态,显著高于浅层土层含水量,其变化范围为10.89%-19.35%,并表现为柠条群落>猪毛蒿群落>蒙古冰草群落>黑沙蒿群落>苜蓿群落。土壤有机碳含量在蒙古冰草群落下为3.505-3.985g/kg,高于其他群落;土壤全氮含量在蒙古冰草、猪毛蒿和柠条群落间差异不显著,为0.146-0.157g/kg,但显著高于黑沙蒿和苜蓿群落。土壤氮矿化过程中,黑沙蒿、柠条和苜蓿样地的土壤硝化作用呈增加趋势,并随季节变化差异增大,而蒙古冰草土壤氮矿化过程则更加平稳,处于较低氮矿化水平的循环特征;相较于柠条和黑沙蒿群落土壤硝化作用对土壤干旱的积极响应,蒙古冰草和苜蓿群落的土壤微生物氮矿化对土壤旱化响应滞后。这5种植物群落土壤氮矿化关键指标主受养分因子影响,在自然降雨和干旱条件下土壤氮与土壤水分、全磷和氮磷比呈正相关,与有机碳和碳氮比负相关,各植物群落土壤铵态氮和硝态氮变化随着持续干旱加剧削弱了与其它养分因子的关联性,但饱和水分后持续干旱的土壤硝态氮和微生物生物量氮呈显著负相关(P<0.05)。

    Abstract:

    In order to explore the responses of soil nitrogen mineralization of common plant communities in the desert grassland of eastern Ningxia to soil drought, five plant communities, namely, Agropyron mongolicum, Artemisia scoparia, Medicago sativa, Caragana korshinskii and Artemisia ordosica were selected to investigate the changes in soil nitrogen mineralization of common plant communities under different soil water gradients (natural, saturated and drought). The results showed that soil moisture of different plant communities was 3.19%-5.17% in 0-20cm soil depth,while the average soil moisture content of each community in 0-200cm depth had all evident vertical dynamics, which were significantly higher than that of shallow soil layer, and its variation range was 10.89%-19.35%, and the sequence was as follows: Caragana korshinskii>Artemisia scoparia>Agropyron mongolicum>Agropyron mongolicum>Medicago sativa. Soil organic carbon content of Agropyron mongolicum was significantly higher than that of other communities and ranged from 3.505g/kg to 3.985g/kg. Soil total nitrogen content did not differ significantly between the community of Agropyron mongolicum, Artemisia scoparia, and Caragana korshinskii, and their value was 0.146-0.157g/kg, but higher than Artemisia ordosica and Medicago sativa. During soil nitrogen mineralization, soil nitrification of Artemisia ordosica, Caragana korshinskii and Medicago sativa community showed an increasing trend, and the difference increased with seasonal variation, whereas soil nitrogen mineralization of Agropyron mongolicum soil was characterized mineralization more stable, and the rate of soil nitrogen mineralization were relatively low. Compared to the positive response of soil nitrification action to soil drought in Caragana korshinskii and Artemisia ordosica community, the responses of soil nitrogen mineralization characteristics in Agropyron mongolicum Medicago sativa community was delayed. The main indices of soil nitrogen mineralisation were influenced by different nutrient factors. Under natural rainfall and drought conditions, soil nitrogen was positively correlated with soil moisture, total phosphorus and the nitrogen to phosphorus ratio, and negatively correlated with organic carbon and the carbon to nitrogen ratio. The changes of soil ammonium and nitrate nitrogen in each plant community weakened the correlations with other nutrient factors as persistent drought intensified, whereas soil nitrate nitrogen and microbial biomass nitrogen showed a significantly negative correlation after persistent drought and saturated moisture(P<0.05).

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李傲天,李志丽,王红梅,刘梦迪.荒漠草原不同植物群落土壤氮矿化对水分梯度的响应.生态学报,2025,45(2):757~768

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