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Atmospheric deposition of inorganic nitrogen in a semi-arid grassland of Inner Mongolia, China 被引量:5
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作者 ZHANG Yibo XU Wen +4 位作者 WEN Zhang WANG Dandan HAO Tianxiang TANG Aohan LIU Xuejun 《Journal of Arid Land》 SCIE CSCD 2017年第6期810-822,共13页
Due to increasing global demand for crop production and energy use, more and more reactive nitrogen(Nr) has been generated and emitted to the environment. As a result, global atmospheric nitrogen(N) deposition has... Due to increasing global demand for crop production and energy use, more and more reactive nitrogen(Nr) has been generated and emitted to the environment. As a result, global atmospheric nitrogen(N) deposition has tripled since the industrial revolution and the ecological environment and human health have been harmed. In this study, we measured dry and wet/bulk N deposition from July 2013 to December 2015 in a semi-arid grassland of Duolun County, Inner Mongolia, China. The samples of dry and wet/bulk N deposition were collected monthly with a DELTA(DEnuder for Long Term Atmospheric sampling) system and with Gradko passive samplers and a precipitation gauge. The measured results show that the annual mean concentrations of NH_3, NO_2, HNO_3, particulate NH_4~+(pNH_4~+) and particulate NO_3^-(pNO_3^-) in atmosphere were 2.33, 1.90, 0.18, 1.42 and 0.42 μg N/m3, respectively, and that the annual mean volume-weighted concentrations of NH_4~+-N and NO_3^--N in precipitation were 2.71 and 1.99 mg N/L, respectively. The concentrations of Nr components(including NH_3, NO_2, HNO_3, p NH_4~+, pNO_3^-, NH_4~+-N and NO_3^--N) exhibited different seasonal variations. Specifically, NO_2 and HNO_3 exhibited higher concentrations in autumn than in summer, while the other Nr components(NH_3, pNH_4~+, pNO_3^-, NH_4~+-N and NO_3^--N) showed the highest values in summer. Based on measured concentrations of Nr components and their deposition velocities estimated using the GEOS-Chem global atmospheric chemical transport model, the calculated annual mean dry deposition fluxes were 3.17, 1.13, 0.63, 0.91 and 0.36 kg N/(hm^2·a) for NH_3, NO_2, HNO_3, p NH_4~+ and pNO_3^-, respectively, and the calculated annual mean wet/bulk deposition fluxes were 5.37 and 3.15 kg N/(hm^2·a) for NH_4~+-N and NO_3^--N, respectively. The estimated annual N deposition(including dry N deposition and wet/bulk N deposition) reached 14.7 kg N/(hm^2·a) in grassland of Duolun County, approaching to the upper limit of the N critical load(10–15 kg N/(hm^2·a)). Dry and wet/bulk deposition fluxes of all Nr components(with an exception of HNO_3) showed similar seasonal variations with the maximum deposition flux in summer and the minimum in winter. Reduced Nr components(e.g., gaseous NH_3 and p NH_4~+ in atmosphere and NH_4~+-N in precipitation) dominated the total N deposition at the sampling site(accounted for 64% of the total N deposition), suggesting that the deposited atmospheric Nr mainly originated from agricultural activities. Considering the projected future increases in crop and livestock production in Inner Mongolia, the ecological and human risks to the negative effects of increased N deposition could be increased if no mitigation measures are taken. 展开更多
关键词 atmospheric reactive nitrogen dry deposition wet/bulk deposition reduced nitrogen grassland ecosystem Inner Mongolia
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Effect of invasion by Hyptis suaveolens on plant diversity and selected soil properties of a constructed tropical grassland
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作者 Talat Afreen Pratap Srivastava +1 位作者 Hema Singh Jamuna Sharan Singh 《Journal of Plant Ecology》 SCIE CSCD 2018年第5期751-760,共10页
Aims Hyptis suaveolens(L.)Poit is an important invader of the tropical and sub-tropical regions of the world.In our study,it has been inves-tigated that how does the H.suaveolens invasion regulate plant spe-cies diver... Aims Hyptis suaveolens(L.)Poit is an important invader of the tropical and sub-tropical regions of the world.In our study,it has been inves-tigated that how does the H.suaveolens invasion regulate plant spe-cies diversity across the seasons in the dry tropical grassland.We hypothesized that a shift in soil inorganic-N availability is caused by invasion,and this shift is integral to access the invasion effect on plant diversity.Methods The study was performed in experimental plots at the Botanical Garden of the Banaras Hindu University(25°16′3.3″N and 82°59′22.7″E),Varanasi,Uttar Pradesh,India.Five replicates(each,2×2m)of non-invaded grassland plots(NIG)and five grassland plots invaded with H.suaveolens(IG)were established.These plots were constructed by transplanting indigenous grassland patches from an adjacent native grassland.In the invaded plots,20 indi-viduals of H.suaveolens were transplanted per plot.After 1 year of establishment,diversity attributes and soil properties were recorded from these plots in three seasons as per standard protocol.Important Findings The results indicated that Hyptis invasion negatively affects plant diversity,with relatively higher impact in rainy season as compared to the winter season.IG exhibited lower soil mois-ture content and temperature than NIG in rainy season,whereas soil ammonium-N,nitrate-N,total inorganic-N,N mineralization registered higher values for IG than NIG in both rainy and win-ter season.Diversity indices were negatively correlated with soil inorganic-N pool and N mineralization.However,these indices were positively correlated with microbial biomass carbon(MBC),and the correlation coefficient for this relationship was higher for rainy season as compared to winter.Species richness(r=0.65)and Shannon diversity(r=0.757)were significantly correlated with the ratio of ammonium-N to nitrate-N.The negative effect of invasion by H.suaveolens on the plant diversity is possibly mediated by the effect of invasion on N mineralization processes(mainly nitrification)and the availability of soil inorganic-N pools.The study indicates that Hyptis invasion has an enormous poten-tial to change the structure and composition of plant communities in the dry tropical grasslands. 展开更多
关键词 dry tropical grassland diversity Hyptis suaveolens MINERALIZATION soil ammonium to nitrate ratio
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