地形对红壤区马尾松林土壤特性与生态化学计量的影响OA
Influences of topography on soil properties and ecological stoichiometry of Pinus massoniana forests in red soil zones
为探究地形因子对红壤区退化地植被持续恢复的影响,以福建长汀典型红壤侵蚀区的朱溪河、罗地河 2 条小流域马尾松林为研究对象,采用公里网格布点法布设样地,调查并测定不同坡度、坡向和海拔马尾松林的土壤理化性质和化学计量特征,分析其与坡度、坡向和海拔等地形因子的关系.结果表明:在 0~20 cm土层,坡度 10°~15°马尾松林土壤的非毛管孔隙度、全钾(TK)、全磷(TP)、全氮(TN)含量显著低于坡度 0°~5°处(P<0.05),而磷钾比(P/K)则相反(P<0.05);阳坡土壤毛管持水量显著高于半阴坡和阴坡(P<0.05);阴坡的土壤TK、速效钾(AK)含量和碳磷比(C/P)及半阴坡的AK含量和速效氮(AN)含量显著高于阳坡(P<0.05),P/K和氮钾比(N/K)则相反(P<0.05);海拔 300~350 m处的土壤最大持水量显著高于海拔 0~300 m;海拔 0~300 m土壤TN、有效磷(AP)、AK含量、P/K和N/K显著低于其他海拔(P<0.05),碳氮比(C/N)和C/P则与之相反(P<0.05).在20~40 cm土层,坡度 10°~15°的马尾松林土壤毛管持水量、AK含量和N/K显著低于其他坡度(P<0.05),AP含量则相反(P<0.05);坡度 0°~5°的马尾松林土壤总有机碳(TOC)含量显著高于坡度10°~15°(P<0.05),TK、TP、AN含量显著高于其他坡度(P<0.05),坡度5°~10°的马尾松林土壤P/K、碳钾比(C/K)显著高于其他坡度(P<0.05);阳坡的毛管孔隙度和N/K显著高于阴坡(P<0.05),阴坡的马尾松林土壤毛管持水量、自然含水量、非毛管孔隙度、TK 含量和 AK 含量、C/K 和 C/N 显著高于阳坡(P<0.05),P/K 则相反(P<0.05);海拔0~300 m土壤毛管持水量、自然含水量、毛管孔隙度和TOC含量显著高于海拔350~400 m(P<0.05),但TK、AP含量显著低于其他海拔(P<0.05),海拔 350~400 m的马尾松林土壤AN含量、P/K、C/K和N/K显著高于其他海拔(P<0.05).随机森林模型表明,影响 0~20 cm土层土壤理化性质和生态化学计量特征的主要地形因子是坡向和海拔,而影响 20~40 cm土层土壤理化性质和生态化学计量特征的主要地形因子则为坡度和坡向.
To investigate the impacts of topographic factors on the sustained recovery of degraded vegetation in red soil zones,this study focused on the Pinus massoniana forests in two small watersheds—the Zhuxi River and Luodi River—in a typical red soil erosion area of Changting,Fujian Province.A kilometer grid sampling method was employed to establish the study plots,and soil physicochemical properties and stoichiometric characteristics were investigated and measured across different slopes,aspects,and altitudes within the P.massoniana forests.The relationships between these parameters and topographic factors such as slope,aspect,and altitude were analyzed.The results indicated that in the 0-20 cm soil layer,the non-capillary porosity,total potassium(TK),total phosphorus(TP),and total nitrogen(TN)content of the P.massoniana forest soil with a slope of 10°-15° were significantly lower than those in the forest with a slope of 0°-5°(P<0.05),while P/K ratio showed the opposite trend(P<0.05).The capillary water holding capacity of the soil on the sunny slope was higher than that on the semi-shady and shady slopes(P<0.05).The TK,available potassium(AK)content,and C/P ratio of the soil on the shady slope and the AK and available nitrogen(AN)content of the soil on the semi-shady slope were higher than those on the sunny slope(P<0.05),while the P/K and N/K ratios exhibited the opposite trend(P<0.05).The maximum water holding capacity of the soil at an altitude of 300-350 m was significantly higher than that at 0-300 m(P<0.05).The TN,available phosphorus(AP),and AK content,as well as the P/K and N/K ratios,of the soil at an altitude of 0-300 m were lower than those at other altitudes(P<0.05),while the C/N and C/P ratios presented the opposite trend(P<0.05).In the 20-40 cm soil layer,the capillary water holding capacity,AK content,and N/K ratio of the P.massoniana forest soil with a slope of 10°-15° were lower than those of the soil with other slopes(P<0.05),while the AP content showcased the opposite trend.The soil with a slope of 0°-5° had higher total organic carbon(TOC)content than that with a slope of 10°-15°(P<0.05)and higher TK,TP,and AN content than that with other slopes(P<0.05).The P/K and C/K ratios of the P.massoniana forest soil with a slope of 5°-10° were higher than those of other slopes(P<0.05).The capillary porosity and N/K ratio of the soil on the sunny slope were significantly higher than those on the shady slope.The capillary water holding capacity,natural water content,non-capillary porosity,TK and AK content,and C/K and C/N ratios of the P.massoniana forest soil on the shady slope were significantly higher than those on the sunny slope,and the P/K ratio demonstrated the opposite trend(P<0.05).The soil at an altitude of 0-300 m had significantly higher capillary water holding capacity,natural water content,capillary porosity,and TOC content than that at 350-400 m and significantly lower TK and AP content than that at other altitudes.The AN content and the P/K,C/K,and N/K ratios of the P.massoniana forest soil at an altitude of 350-400 m were higher than those at other altitudes(P<0.05).The random forest model indicated that the main factors influencing the soil physical and chemical properties and ecological stoichiometric characteristics in the 0-20 cm soil layer are aspect and altitude,while the main factors influencing those in the 20-40 cm soil layer are slope and aspect.
WANG Xiaoyu;YUAN Yuqi;LI Yijie;HUANG Siqi;CUI Yongsheng;HOU Xiaolong
College of Forestry,Fujian Agriculture and Forestry University,Fuzhou,Fujian 350002,ChinaCollege of Forestry,Fujian Agriculture and Forestry University,Fuzhou,Fujian 350002,ChinaCollege of Forestry,Fujian Agriculture and Forestry University,Fuzhou,Fujian 350002,ChinaCollege of Forestry,Fujian Agriculture and Forestry University,Fuzhou,Fujian 350002,ChinaCollege of Forestry,Fujian Agriculture and Forestry University,Fuzhou,Fujian 350002,China||Cross-Strait Red Soil and Water Conservation Collaborative Innovation Center,Fuzhou,Fujian 350002,ChinaCollege of Forestry,Fujian Agriculture and Forestry University,Fuzhou,Fujian 350002,China||National Positioning Observatory of Red Loam Hilly Ecosystem,Changting,Fujian 366300,China
农业科技
坡度坡向红壤区马尾松海拔土壤生态化学计量
slopeaspectred soil zonePinus massonianaaltitudesoil ecological stoichiometry
《森林与环境学报》 2026 (1)
30-39,10
国家重点研发计划项目"马尾松人工林林下覆被诱导恢复与土壤侵蚀控制技术"(2023YFF130440304)国家自然科学基金项目"基于移地试验研究土壤'微生物碳泵'和'矿物碳泵'的协同固碳机制"(32371853).
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