The typical steppe ecosystems in China are now being increasingly degraded due mainly toovergrazing. To determine the limiting nutrients is of significance in order to find out ways of successfullyrestoring the degrad...The typical steppe ecosystems in China are now being increasingly degraded due mainly toovergrazing. To determine the limiting nutrients is of significance in order to find out ways of successfullyrestoring the degraded steppe. In addition to field fertilization experiments, N:P stoichiometry is an alternative,but argumentative tool to study nutrient limitation. In this study, we used these two approaches to identifythe most limiting nutrient element at the species level. Furthermore, nutrient addition experimentprovides an effective means to test our hypothesis that N:P stoichiometry will remain constant becauserelatively narrow range of N:P ratio in tissues of the terrestrial plants is an important adaptive mechanismfor plants to survive on earth. For these purposes, we designed a field experiment to examine theresponses of biomass and N:P stoichiometry of the two dominant species -- Leyrnus chinensis (Trin.)Tzvel. and Carex korshinskyiKom. -- to N fertilization at rates of O, 5, 15, 30, 50 and 80 g NH4NO3.m-2.a-~in two adjacent sites, one being excluded animal grazing for 22 years (site A), and another being free ofgrazing for only two years (site B) before the experiment was carried out. No effects of N fertilization weredetected in the first year as reflected by the aboveground biomass and P concentrations of the twospecies. The regression analysis showed that N:P ratios of two species of both sites remained constant inthe second year. N fertilization significantly increased the N concentrations of two species in both years,while only significantly increased the P contents of the two species in the second year. N and P contentsof the two species were significantly correlated in all cases in 2001. Our results suggest that theL. chinensis was in short of N in site B while the growth of C. korshinskyi was limited by P in site A, andthere is a significant synergistic relationship between tissue N and P concentrations in 2001. Our hypothesiswas valid on the species level since N:P ratio of the two species remaine展开更多
氮沉降的增加显著改变了生态系统功能和过程。大量研究表明,氮添加会提高生态系统生产力,然而,大部分研究集中在地上生物量,对地下生物量以及根冠比的研究较少。我们在内蒙古典型草原进行了7年的氮添加实验,设置6个氮添加水平,分别是N0...氮沉降的增加显著改变了生态系统功能和过程。大量研究表明,氮添加会提高生态系统生产力,然而,大部分研究集中在地上生物量,对地下生物量以及根冠比的研究较少。我们在内蒙古典型草原进行了7年的氮添加实验,设置6个氮添加水平,分别是N0(0)、N1(5.6 g N·m^-2)、N2(11.2 g N·m^-2)、N3(22.4 g N·m^-2)、N4(39.2 g N·m^-2)、N5(56 g N·m^-2),测定植物地上和不同土层(0~10、10~30、30~50和50~100 cm)地下生物量并计算根冠比,研究不同氮添加水平对植物地上、地下生物量和根冠比的影响。结果表明:(1)与对照相比,低氮添加水平(N1和N2)未显著增加地上生物量,高氮添加水平(N3~N5)显著增加了地上生物量(96%~117%),且各高氮添加水平间差异不显著;(2)不同氮添加水平下,植物地上生物量的氮响应效率(NRE)均大于0且呈下降趋势,相邻氮添加水平的NRE差值(ΔNRE)仅在N3水平下显著增加,说明地上生物量在N3水平下达到饱和;(3)氮添加未显著改变不同土层以及整个土壤剖面上的地下生物量,且对各土层地下生物量的占比情况无显著影响;(4)与对照相比,N1和N2未显著改变植物的根冠比,N3~N5显著降低了植物根冠比。综上所述,氮沉降增加会提高植物地上生物量,对不同土层根系的影响比较复杂,需要更多的研究来明确地下生产力对氮沉降增加的响应规律。展开更多
文摘The typical steppe ecosystems in China are now being increasingly degraded due mainly toovergrazing. To determine the limiting nutrients is of significance in order to find out ways of successfullyrestoring the degraded steppe. In addition to field fertilization experiments, N:P stoichiometry is an alternative,but argumentative tool to study nutrient limitation. In this study, we used these two approaches to identifythe most limiting nutrient element at the species level. Furthermore, nutrient addition experimentprovides an effective means to test our hypothesis that N:P stoichiometry will remain constant becauserelatively narrow range of N:P ratio in tissues of the terrestrial plants is an important adaptive mechanismfor plants to survive on earth. For these purposes, we designed a field experiment to examine theresponses of biomass and N:P stoichiometry of the two dominant species -- Leyrnus chinensis (Trin.)Tzvel. and Carex korshinskyiKom. -- to N fertilization at rates of O, 5, 15, 30, 50 and 80 g NH4NO3.m-2.a-~in two adjacent sites, one being excluded animal grazing for 22 years (site A), and another being free ofgrazing for only two years (site B) before the experiment was carried out. No effects of N fertilization weredetected in the first year as reflected by the aboveground biomass and P concentrations of the twospecies. The regression analysis showed that N:P ratios of two species of both sites remained constant inthe second year. N fertilization significantly increased the N concentrations of two species in both years,while only significantly increased the P contents of the two species in the second year. N and P contentsof the two species were significantly correlated in all cases in 2001. Our results suggest that theL. chinensis was in short of N in site B while the growth of C. korshinskyi was limited by P in site A, andthere is a significant synergistic relationship between tissue N and P concentrations in 2001. Our hypothesiswas valid on the species level since N:P ratio of the two species remaine
文摘氮沉降的增加显著改变了生态系统功能和过程。大量研究表明,氮添加会提高生态系统生产力,然而,大部分研究集中在地上生物量,对地下生物量以及根冠比的研究较少。我们在内蒙古典型草原进行了7年的氮添加实验,设置6个氮添加水平,分别是N0(0)、N1(5.6 g N·m^-2)、N2(11.2 g N·m^-2)、N3(22.4 g N·m^-2)、N4(39.2 g N·m^-2)、N5(56 g N·m^-2),测定植物地上和不同土层(0~10、10~30、30~50和50~100 cm)地下生物量并计算根冠比,研究不同氮添加水平对植物地上、地下生物量和根冠比的影响。结果表明:(1)与对照相比,低氮添加水平(N1和N2)未显著增加地上生物量,高氮添加水平(N3~N5)显著增加了地上生物量(96%~117%),且各高氮添加水平间差异不显著;(2)不同氮添加水平下,植物地上生物量的氮响应效率(NRE)均大于0且呈下降趋势,相邻氮添加水平的NRE差值(ΔNRE)仅在N3水平下显著增加,说明地上生物量在N3水平下达到饱和;(3)氮添加未显著改变不同土层以及整个土壤剖面上的地下生物量,且对各土层地下生物量的占比情况无显著影响;(4)与对照相比,N1和N2未显著改变植物的根冠比,N3~N5显著降低了植物根冠比。综上所述,氮沉降增加会提高植物地上生物量,对不同土层根系的影响比较复杂,需要更多的研究来明确地下生产力对氮沉降增加的响应规律。
