首页|增温和降水变化对陇中黄土高原半干旱麦田土壤有机碳和酶活性的影响

增温和降水变化对陇中黄土高原半干旱麦田土壤有机碳和酶活性的影响

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农田生态系统受气候变化影响强烈,但全球变暖和降水变化及其交互作用对农田土壤有机碳和酶活性的影响及两者的关系仍缺乏认知。本研究依托开顶式气室(OTC)增温平台和降水控制平台,以陇中黄土高原半干旱春小麦农田为研究对象,研究增温和降水变化及其耦合对土壤有机碳和酶活性的影响。试验共设置6个处理:对照(CK)、减水30%(-P30)、增水30%(+P30)、增温(W)、增温减水30%(W-P30)、增温增水30%(W+P30)。结果表明:OTC增温显著提高了土壤有机碳(SOC)、微生物生物量碳(MBC)、易氧化有机碳(KMnO4-C)、溶解性有机碳(DOC)和颗粒态有机碳(POC)含量,而矿物结合态有机碳(MAOC)含量变化不显著。自然温度条件下,增减雨处理均未显著改变土壤有机碳组分含量;而在增温条件下,增加降水量显著提高了 DOC和POC含量;增温与降水交互作用显著影响了 SOC、DOC和KMnO4-C含量。增温和增加降水及两者交互增加了碳库管理指数(CMI)、碳库指数(CPI)、土壤纤维二糖水解酶、脲酶、蔗糖酶、N-乙酰-β-D-葡萄糖苷酶活性和作物生物量。土壤温度、土壤水分与土壤有机碳组分和酶活性均呈正相关(除土壤温度和蔗糖酶活性呈负相关外)。随机森林模型分析表明,土壤理化性质、酶活性、温度和含水量解释了 SOC、MBC、POC、KMnO4-C和DOC含量变化的52。4%~71。1%,其中相关重要性较高的5个因子分别为土壤脲酶活性、土壤温度、土壤水分、土壤N-乙酰-β-D-葡萄糖苷酶活性和有效磷。然而,各因子对MAOC含量变化的解释度较低(21。5%)。综上,增温和降水变化会显著影响陇中黄土高原旱地麦田土壤性质、酶活性和作物生物量,从而影响土壤有机碳库。
Effects of warming and precipitation changes on soil organic carbon and enzyme activities in semi-arid wheatland fields on the Loess Plateau of central Gansu Province,China
Farmland ecosystems are strongly affected by climate change,but the effects of global warming and pre-cipitation changes and their interactions on soil organic carbon and enzyme activities in farmland soils and their rela-tionships are still poorly understood.In this study,we employed the Open-Top Chamber(OTC)warming platform and the precipitation manipulative platform to investigate the effects of warming and precipitation changes on soil organic carbon and enzyme activities in semi-arid spring wheat farmland in Loess Plateau of the central Gansu Pro-vince.There were six treatments:control(CK),30%precipitation reduction(-P30),30%precipitation increase(+P30),warming(W),warming and 30%precipitation reduction(W-P30),and warming and 30%precipitation increase(W+P30).The results showed that OTC warming significantly elevated soil organic carbon(SOC),micro-bial biomass carbon(MBC),readily oxidizable organic carbon(KMnO4-C),dissolved organic carbon(DOC),and particulate organic carbon(POC)contents.In contrast,the mineral associated organic carbon(MAOC)con-tent changed little.Under ambient temperature,neither an increase nor a decrease in precipitation resulted in a sig-nificant alteration of soil organic carbon fractions.However,under the warming condition,elevated precipitation resulted in a notable enhancement in DOC and POC contents.Warming and precipitation significantly interacted to affect SOC,DOC,and KMnO4-C contents.The interaction between precipitation and warming resulted in an increase in the carbon pool management index(CMI),the carbon pool index(CPI),the activity of soil cellobiose hydrolase,urease,sucrase,N-acetyl-β-D-glucosidase,as well as crop biomass.The correlations between soil tem-perature,moisture,soil organic carbon fractions and enzyme activities were positive.There was a negative correla-tion between soil temperature and sucrase activity.The random forest modelling analysis demonstrated that soil physicochemical properties,enzyme activities,temperature and water content together explained 52.4%to 71.1%,and the five factors with higher correlation importance were soil urease activity,soil temperature,soil moisture,soil N-acetyl-β-D-glucosidase activity,and effective phosphorus.However,the selected factors only accounted for 21.5%of the observed variation in MAOC content.In conclusion,warming and precipitation changes significantly affected soil properties,enzyme activities and crop biomass,and thus soil organic carbon pools,in semi-arid wheat-land soil of Loess Plateau of central Gansu Province.

warmingprecipitation changewheatland soilorganic carbon fractionenzyme activity

张鹏、田瑞、胡啸、赵同亮、雷俊、王鹤龄、吕晓东

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兰州交通大学环境与市政工程学院,兰州 730070

中国气象局兰州干旱气象研究所中国气象局干旱气候变化与减灾重点开放实验室,兰州 730020

祁连山中部亚高山生态系统野外科学观测研究站,甘肃张掖 734000

增温 降水变化 麦田土壤 有机碳组分 酶活性

2024

应用生态学报
中国生态学学会 中国科学院沈阳应用生态研究所

应用生态学报

CSTPCD北大核心
影响因子:2.114
ISSN:1001-9332
年,卷(期):2024.35(11)