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.
Peng Zhang, Rui Tian, H U Hu, Tong-Liang Zhao, Jun Lei, He-Ling Wang
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引用次数: 0
Abstract
Farmland ecosystems are strongly affected by climate change, but the effects of global warming and precipitation changes and their interactions on soil organic carbon and enzyme activities in farmland soils and their relationships 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), microbial 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) content changed little. Under ambient temperature, neither an increase nor a decrease in precipitation resulted in a significant 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 temperature, moisture, soil organic carbon fractions and enzyme activities were positive. There was a negative correlation 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 wheatland soil of Loess Plateau of central Gansu Province.
气候变化对农田生态系统的影响较大,但全球变暖和降水变化及其相互作用对农田土壤有机碳和酶活性的影响及其相互关系尚不清楚。本研究采用开放式顶室(OTC)增温平台和降水操纵平台,研究了增温和降水变化对甘中黄土高原半干旱春小麦农田土壤有机碳和酶活性的影响。6个处理:对照(CK)、减少30%降水(-P30)、增加30%降水(+P30)、增温(W)、增温+减少30%降水(W-P30)、增温+增加30%降水(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)、溶解有机碳(DOC)和颗粒有机碳(POC)含量;而矿物伴生有机碳(MAOC)含量变化不大。在环境温度下,降水量的增加和减少都没有引起土壤有机碳组分的显著变化。增温条件下,降水增加导致DOC和POC含量显著增加。增温和降水对土壤有机碳、DOC和KMnO4-C含量影响显著。降水与增温的交互作用导致碳库管理指数(CMI)、碳库指数(CPI)、土壤纤维素二糖水解酶、脲酶、蔗糖酶、n -乙酰-β- d -葡萄糖苷酶活性和作物生物量增加。土壤温度、湿度、土壤有机碳组分与酶活性呈显著正相关。土壤温度与蔗糖酶活性呈负相关。随机森林模型分析表明,土壤理化性质、酶活性、温度和含水量共同解释52.4% ~ 71.1%,相关性较高的5个因子分别是土壤脲酶活性、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,所选因子仅占观测到的MAOC含量变化的21.5%。综上所述,增温和降水变化显著影响了陇中黄土高原半干旱麦田土壤的土壤性质、酶活性和作物生物量,进而影响了土壤有机碳库。