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A meta-analysis of soil salinization effects on nitrogen pools, cycles and fluxes in coastal ecosystems

机译:沿海生态系统中氮素池,循环和助熔剂的土壤盐渍化作用的荟萃分析

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Salinity intrusion caused by land subsidence resulting from increasing groundwater abstraction, decreasing river sediment loads and increasing sea level because of climate change has caused widespread soil salinization in coastal ecosystems. Soil salinization may greatly alter nitrogen (N) cycling in coastal ecosystems. However, a comprehensive understanding of the effects of soil salinization on ecosystem N pools, cycling processes and fluxes is not available for coastal ecosystems. Therefore, we compiled data from 551 observations from 21 peer-reviewed papers and conducted a meta- analysis of experimental soil salinization effects on 19 variables related to N pools, cycling processes and fluxes in coastal ecosystems. Our results showed that the effects of soil salinization varied across different ecosystem types and salinity levels. Soil salinization increased plant N content (18%), soil NH4+ (12%) and soil total N (210%), although it decreased soil NO3- (2%) and soil microbial biomass N (74%). Increasing soil salinity stimulated soil N2O fluxes as well as hydrological NH4+ and NO2- fluxes more than threefold, although it decreased the hydrological dissolved organic nitrogen (DON) flux (59%). Soil salinization also increased the net N mineralization by 70%, although salinization effects were not observed on the net nitrification, denitrification and dissimilatory nitrate reduction to ammonium in this meta-analysis. Overall, this meta-analysis improves our understanding of the responses of ecosystem N cycling to soil salinization, identifies knowledge gaps and highlights the urgent need for studies on the effects of soil salinization on coastal agro-ecosystem and microbial N immobilization. Additional increases in knowledge are critical for designing sustainable adaptation measures to the predicted intrusion of salinity intrusion so that the productivity of coastal agro-ecosystems can be maintained or improved and the N losses and pollution of the natural environment can be minimized.
机译:由于气候变化增加了地下水抽取,降低河水沉积物,降低河泥浆负荷和增加海平面引起的盐度入侵引起的沿海生态系统引起了广泛的土壤盐渍化。土壤盐渍化可能大大改变沿海生态系统的循环氮气(n)。然而,沿海生态系统无法全面了解土壤盐渍化对生态系统的影响,骑自行车的过程和助体。因此,我们从21个同行评审纸中编制了551个观察的数据,并对与N个池,沿海生态系统中的N个池,循环过程和助熔剂有关的19个变量进行了对实验土壤盐渍化影响的荟萃分析。我们的研究结果表明,土壤盐渍化对不同生态系统类型和盐度水平的影响变化。土壤盐渍化增加植物N含量(18%),土壤NH4 +(12%)和土壤总计N(210%),尽管土壤下降1号(2%)和土壤微生物生物量N(74%)。增加土壤盐度刺激的土壤N2O助熔剂以及水文NH4 +和NO 2-助焊剂,虽然它降低了水文溶解的有机氮(DON)通量(59%)。土壤盐渍化也增加了70%的净矿化,尽管在该荟萃分析中未观察到净硝化,脱氮和硝酸硝酸盐还原对铵盐的碳化效应。总体而言,这种元分析改善了我们对生态系统N循环到土壤盐渍化的反应的理解,确定了知识差距,并突出了对土壤盐渍化对沿海农业生态系统和微生物N固定的影响的迫切需要。知识的额外增加对于为预测盐度入侵的可持续措施设计可持续适应措施至关重要,以便维持或改善沿海农业生态系统的生产率,并且可以最小化自然环境的N损失和污染。

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