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1. 中国科学院水利部水土保持研究所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌,712100
2. 中国科学院大学,北京,100049
3. 西北农林科技大学资源与环境学院, 陕西 杨凌,712100
4. 西北农林科技大学水土保持研究所, 陕西 杨凌,712100
Published:2021
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WANG Mei, YAN Ziran, ZHAO Ziwen, et al. Variation Characteristics of Specific Soil Enzyme Activities During Vegetation Succession on the Loess Plateau[J]. 2021, 35(5): 181-187.
WANG Mei, YAN Ziran, ZHAO Ziwen, et al. Variation Characteristics of Specific Soil Enzyme Activities During Vegetation Succession on the Loess Plateau[J]. 2021, 35(5): 181-187. DOI: 10.13870/j.cnki.stbcxb.2021.05.025.
明确土壤相对酶活性在植被恢复过程中的变化特征及影响因素,对客观揭示植被次生演替过程中微生物活性变化特征具有重要意义。利用时空互代法,选取黄土丘陵区植被次生演替过程中农田、草地、灌木、先锋林和顶级群落5个阶段为研究对象,探讨了β-1,4-葡萄糖苷酶(BG)、纤维二糖水解酶(CBH)、β-木糖苷酶(BX)、N-乙酰-β-D-氨基葡萄糖苷酶(NAG)、亮氨酸氨基肽酶(LAP)、丙氨酸酶转氨酶(ALT)和碱性磷酸酶(AP)7种酶活性变化特征及影响因素。结果表明:在植被次生演替过程中,单位土壤有机碳(SOC)、土壤CBH、BX和NAG酶活性伴随植被次生演替先显著升高后显著降低(P<0.05),并在先锋林阶段达到最高点;单位土壤微生物磷脂脂肪酸(PLFA)的3种酶活性呈现相反趋势,并在顶级群落阶段最高。相关性分析显示,单位SOC和PLFA土壤CBH、BX和NAG酶活性均与土壤pH显著负相关且与土壤DOC显著正相关(P<0.05);单位SOC和PLFA土壤相对酶活性分别与土壤生物因子显著的正相关和负相关(P<0.05)。冗余分析表明,土壤中磷含量和碳氮含量分别是单位SOC和单位PLFA土壤相对酶活性变化主要驱动因子。研究结果为进一步揭示次生演替过程中土壤养分循环和质量变化提供新的见解。
Clarifying the characteristics and influencing factors of specific soil enzyme activities in the process of vegetation restoration is of great significance to objectively revealing the change characteristics of microbial activity in the process of vegetation secondary succession. Based on the method of spatiotemporal interaction
this study selected five stages in the vegetation secondary succession process in the loess hilly region as the research objects
including farmland
grassland
shrubs
pioneer forests and top community stage
and discussed the change characteristics and influencing factors of specific soil enzyme activities of seven enzymes (β-1
4-glucose Glucosidase (BG)
cellobio hydrolase (CBH)
β-xylosidase (BX)
N-acetyl-beta-D-glucosaminidase (NAG)
leucine amino peptide (LAP)
alaninase transaminase (ALT)) and alkaline phosphatase (AP)). The results showed that in the process of vegetation secondary succession
unit soil organic carbon (SOC)
soil CBH
BX and NAG activities increased significantly at first and then decreased significantly (P < 0.05)
and it reached the highest point in the pioneer forest stage; while the activities of three enzymes per unit soil microbial phospholipid fatty acid (PLFA) showed opposite trends (P < 0.05)
and reached the highest level in the top community stage. Correlation analysis showed that soil CBH
BX and NAG enzyme activities per unit SOC and PLFA were significantly negatively correlated with soil pH and significantly positively correlated with soil DOC (P < 0.05); specific soil enzyme activity per unit SOC and PLFA were significantly positively correlated and negatively correlated with soil biological factors
respectively (P < 0.05). Redundancy analysis showed that the phosphorus content as well as the carbon and nitrogen content in the soil were the main driving factor for the change of specific enzyme activity per SOC and PLFA
respectively. This study provided new information for further revealing the soil nutrient cycling and quality changes during the secondary succession process.
Jong R D, Bruin S D, Schaepman M, et al. Quantitative mapping of global land degradation using Earth observations[J]. International Journal of Remote Sensing, 2011, 32(21):6823-6853.
Nadal-Romero E, Cammeraat E, Perez-Cardie E, et al. Effects of secondary succession and afforestation practices on soil properties after cropland abandonment in humid Mediterranean mountain areas[J]. Agriculture, Ecosystems and Environment, 2016, 228:91-100.
Van Hall R L, Cammeraat L H, Keesstra S D, et al. Impact of secondary vegetation succession on soil quality in a humid Mediterranean landscape[J]. Catena, 2017, 149:836-843.
赵子文, 王国梁, 吴阳, 等.黄土高原不同植被带人工刺槐林土壤氮磷转化酶动力学参数及其温度敏感性[J]. 应用生态学报, 2020, 31(8):2515-2522.
Ma W J, Li J, Gao Y, et al. Responses of soil etracellular enzyme activities and microbial community properties to interaction between nitrogen addition and increased precipitation in a semi-arid grassland ecosystem[J]. Science of the Total Environment, 2020, 703:e134691.
Raiesi F, Beheshti A. Soil specific enzyme activity shows more clearly soil responses to paddy rice cultivation than absolute enzyme activity in primary forests of northwest Iran[J]. Applied Soil Ecology, 2014, 75:63-70.
Zhang X Y, Dong W Y, Dai X Q, et al. Responses of absolute and specific soil enzyme activities to long term additions of organic and mineral fertilizer[J]. Science of the Total Environment, 2015, 536:59-67.
Yu P J, Tang X G, Zhang A C, et al. Responses of soil specific enzyme activities to short-term land use conversions in a salt-affected region, northeastern China[J]. Science of the Total Environment, 2019, 687:939-945.
Liu X, Guo K L, Huang L, et al. Responses of absolute and specific enzyme activity to consecutive application of composted sewage sludge in a Fluventic Ustochrept[J]. PLoS One, 2017, 12(5):e017776.
邹厚远, 刘国彬, 王晗生.子午岭林区北部近50年植被的变化发展[J]. 西北植物学报, 2002, 22(1):1-8.
Wang Y Q, Shao M A, Shao H B. A preliminary investigation of the dynamic characteristics of dried soil layers on the Loess Plateau of China[J]. Journal of Hydrology, 2010, 381(1/2):9-17.
Wang K B, Shao R X, Shangguan Z P. Changes in species richness and community productivity during succession on the Loess Plateau (China)[J]. Polish Journal of Ecology, 2010, 58(3):501-510.
鲍士旦.土壤农化分析[M]. 3版.北京:中国农业出版社, 2000.
Bligh E G, Dyer W J. A rapid method of total lipid extraction and purification[J]. Canadian Journal of Biochemistry and Physiology, 1959, 37(8):911-917.
Marx M C, Kandeler E, Wood M, et al. Exploring the enzymatic landscape:Distribution and kinetics of hydrolytic enzymes in soil particle-size fractions[J]. Soil Biology and Biochemistry, 2005, 37(1):35-48.
蒲琴, 胡玉福, 何剑锋, 等.植被恢复模式对川西北沙化草地土壤微生物量及酶活性研究[J]. 水土保持学报, 2016, 30(4):323-328.
Medeiros E V, Duda G P, Rodrigues dos Santos L A, et al. Soil organic carbon, microbial biomass and enzyme activities responses to natural regeneration in a tropical dry region in Northeast Brazil[J]. Catena, 2017, 151:137-146.
Davidson E A, Janssens I A, Luo Y. On the variability of respiration in terrestrial ecosystems:Moving beyond Q10[J]. Global Change Biology, 2006, 12(2):154-164.
Treseder K K and Vitousek P M. Effects of soil nutrient availability on investment in acquisition of N and P in Hawaiian rain forests[J]. Ecology, 2001, 82(4):946-954.
Cui Y X, Wang X, Zhang X C, et al. Soil moisture mediates microbial carbon and phosphorus metabolism during vegetation succession in a semiarid region[J]. Soil Biology and Biochemistry, 2020, 147:1-11.
薛萐, 刘国彬, 戴全厚, 等.黄土丘陵区人工灌木林恢复过程中的土壤微生物生物量演变[J]. 应用生态学报, 2008, 19(3):517-523.
姜华, 毕玉芬, 朱栋斌, 等.恢复措施对云南退化山地草甸土壤微生物和酶活性的影响[J]. 草地学报, 2008, 16(3):256-261.
Xiao W, Chen X, Jing X, et al. A meta-analysis of soil extracellular enzyme activities in response to global change[J]. Soil Biology and Biochemistry, 2018, 123:21-32.
Kuzyakov Y, Raskatov A, Kaupenjohann M. Turnover and distribution of root exudates of
Zea mays
. Plant and Soil, 2003, 254(1/2):317-327.
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