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土壤碳氮磷和酶化学计量特征对原始林转换的响应

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为了解区域典型农林用地土壤碳、氮、磷、胞外酶生态化学计量特征,采用时空代换法研究湘西北本底一致、土地利用史清晰的常绿阔叶原始林及其转换而来的人工林地、果园、坡耕地和水田0~40 cm土层中有机碳含量、全氮含量、全磷含量、胞外酶活性、计量比值及其与活性碳、氮、磷组分的关系.结果表明,与原始林相比,果园和坡耕地土壤有机碳、全氮、全磷含量的降幅(40%~79%)较高,且深层土壤(20~40 cm)和表土(0~20 cm)的降幅类似,表明原始林转换为果园、坡耕地不利于深层土壤有机碳和养分的保存.果园、坡耕地、水田和原始林土壤碳、氮、磷含量的比值无显著差异.杉木人工林土壤碳、氮、磷含量比值较原始林高60%~124%,说明人工林土壤存在较强的氮、磷素共同限制作用.与原始林相比,土地利用方式转换后,土壤胞外酶活性降低 18%~64%;果园和坡耕地表土碳磷获取酶计量比(EC/P)也显著降低,而深层土壤EC/P显著升高.土壤中碳含量、氮含量、磷含量、酶活性及其计量比值与活性碳、氮、磷组分含量显著相关.原始林转换导致表土和深层土壤中的碳含量、氮含量、磷含量、胞外酶活性大幅下降,微生物底物有效性降低,表明土壤质量/健康退化.土壤碳、氮、磷含量计量比和酶计量比值对原始林转换的响应较弱,对土壤健康的指示作用有待进一步探索.
Responses of soil C,N,P,and enzyme stoichiometry to primary forest conversion
To elucidate the stoichiometric dynamics of organic C,N,P,and extracellular enzymes in soil in typical agricultural and forestry lands,primary evergreen broad-leaved forests and converted plantations,orchards,sloping croplands,and paddies with similar geographical backgrounds and clear land-use history in western Hunan Province were selected.The space-for-time substitution method was applied to reveal the effect of primary forest conversion on the contents of organic C,total N,and total P;activities of extracellular enzymes,including their:stoichiometric ratios;relationships with labile C,N,and P fractions at a soil depth of 0-40 cm.Compared to the primary forest,the contents of soil organic C,total N,and total P in the orchard and sloping cropland were much more greatly reduced(40%-79%)than that in plantations and paddies.The reduction was similar in topsoil and deep soil,indicating relatively unfavorable conditions for organic C and nutrient preservation in deep soil under orchards and sloping croplands.No significant differences in soil C-N-P ratios were observed among the orchards,sloping croplands,paddy fields,and primary forests.The C-N-P ratios in soil were 60%-124%higher in plantations than in primary forests,indicating co-limitation by N and P in the soil under the plantation.The β-glucosaminidase,β-N-acetyl glucosaminidase,leucine aminopeptidase,and acid phosphatase activities were reduced by 18%-64%in the converted land-use sites than in the primary forest.Compared to that of the primary forest,the stoichiometric ratios of C-and P-acquiring enzyme(EC/P)in the topsoil under the orchard and sloping cropland were significantly reduced,whereas the EC/P ratios in the 20-40 cm deep soil were significantly increased.The contents of organic C,total N,total P,enzyme activities,and their ratios were significantly correlated with the contents of the labile C,N,and P fractions in soil.Primary forest conversion resulted in substantial reductions in soil organic C,total N,and total P contents and extracellular enzyme activities in the topsoil and at depths of 20-40 cm deep.This indicates a reduction in microbial substrate availability and soil quality/health degradation.The responses of the stoichiometric ratios of soil organic C,total N,and total P contents and enzyme activities to primary forest conversion were relatively weak.Whether these stoichiometric ratios can effectively indicate the soil health change remains further exploration.

northwestern Hunan provincedeep soilsoil nutrientecological stoichiometryextracellular enzyme activityland use

肖华翠、梁万栋、李源钊、盛浩、周萍

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湖南农业大学资源学院,湖南 长沙 410128

中国科学院亚热带农业生态研究所亚热带农业生态过程重点实验室,湖南 长沙 410125

湘西北 深层土壤 土壤养分 生态化学计量学 胞外酶活性 土地利用

湖南省重点研发计划国家自然科学基金科技基础资源调查专项

2023NK2026415712342021FY100504

2024

森林与环境学报
福建农林大学

森林与环境学报

CSTPCD北大核心
影响因子:0.964
ISSN:2096-0018
年,卷(期):2024.44(3)
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