
西南喀斯特地区马尾松人工林林龄对土壤理化性质的影响
武燕, 黄青, 刘讯, 郑睿, 岑佳宝, 丁波, 张运林, 符裕红
南京林业大学学报(自然科学版) ›› 2024, Vol. 48 ›› Issue (3) : 99-107.
西南喀斯特地区马尾松人工林林龄对土壤理化性质的影响
Effects of Pinus massoniana plantation age on soil physical and chemical properties in Karst areas in southwest China
【目的】 了解西南喀斯特地区不同龄组马尾松(Pinus massoniana)人工林土壤理化性质变化,综合分析地形因子、林分特征及植物多样性指标对土壤性质的影响,为退化喀斯特地区环境治理提供参考。【方法】 在贵州省遵义市凤冈县,选取中龄林、近熟林和过成熟林3个龄组系列共11个马尾松人工林样地,样地按25.82 m×25.82 m方形设置,调查乔木层植物种名、高度及胸径,同时记录样地海拔、坡位、坡度及各样地主要物种组成,在每个样地的西南、西北、东北、东南、中共5个方位设置5个2 m×2 m的灌木样方,调查灌木层植物种名及株数,在每个灌木样方内设置1 m×1 m的草本样方,调查草本层植物种名和盖度,量化马尾松人工林土壤理化性质变化并分析其影响因子。【结果】 不同龄组之间马尾松人工林土壤容重、孔隙度、含水量、有机碳含量、全磷含量均无显著差异(P>0.05),而全氮含量在[0,20)cm土层随林龄的增长呈先升高后降低,碱解氮含量在[20,40)cm土层随林龄的增长逐步降低,速效磷含量在[0,20)cm和[20,40)cm土层随林龄的增长呈先降低后升高的趋势(P<0.05);马尾松人工林土壤容重、孔隙度和含水量在同一龄组[0,20)cm和[20,40)cm的两土层之间均无显著差异(P>0.05),中龄林、近熟林和过成熟林的土壤有机碳含量、近熟林和过成熟林的全氮含量和碱解氮含量、过成熟林的全磷含量和速效磷含量在[0,20)cm和[20,40)cm两土层之间均有显著差异(P<0.05),均随土层的加深而降低;相关性分析表明,地形因子、林分特征和植物多样性指标均是影响马尾松人工林土壤物理性质和养分变化的因素,逐步回归分析显示影响土壤物理性质变化的因素主要是林分密度和植物多样性指标,而地形因子、林分特征和植物多样性均是影响土壤养分的因素。RDA分析表明林分特征解释马尾松人工林土壤理化性质变异的36.60%,植物多样性解释土壤理化性质变异的27.00%,地形因子解释土壤理化性质变异的10.30%。【结论】 龄组变化对马尾松人工林土壤氮磷含量产生了显著影响,马尾松人工林的经营管理过程中应随着马尾松的生长发育适当添加氮肥和磷肥以维持马尾松人工林的生产力和可持续发展,而龄组变化对土壤物理性质没有显著影响,林分密度和树高是影响土壤理化性质变化的主要因子。
【Objective】 The aim of the present study was to investigate the changes of soil physical and chemical properties of Pinus massoniana plantations of different ages in Karst areas in southwest China, as well as comprehensively analyze the effects of topographic factors, stand characteristics and plant diversity on soil properties to provide reference for environmental management in degraded Karst areas.【Method】 In the present study, 11 P. massoniana plantations at three different ages, namely, middle-aged plantation, near-mature plantation, and over-aged plantation, were selected in Fenggang County, Zunyi City, Guizhou Province. The area of the plots was 25.82 m × 25.82 m. The species name, height and diameter at breast height (DBH) of the tree layer were investigated, and the altitude, position, slope and species composition of each plot were recorded. Five 2 m × 2 m shrub quadrats were set up in the southwest, northwest, northeast, southeast and middle areas of each plot to investigate the species name and number of plants in the shrub layer. A 1 m × 1 m herb quadrat was set up in each shrub quadrat to investigate the species name and coverage of herbs. The changes of soil physical and chemical properties were quantified, and the influencing factors were analyzed.【Result】 There were no significant differences in soil bulk density, porosity, water content, organic carbon content and total phosphorus content among the different age groups of the P. massoniana plantations (P>0.05). The total nitrogen content increased initially and then decreased with the increase in plantation age in the 0-20 cm soil layer, and the alkali-hydrolyzable nitrogen content decreased gradually with the increase of plantation age in the 20-40 cm soil layer. Moreover, the available phosphorus content decreased initially and then increased with the increase in plantation age in the 0-20 cm and 20-40 cm soil layers (P<0.05). No significant differences were found in the soil bulk density, porosity, and water content between the 0-20 cm and 20-40 cm soil layers within the same age group (P>0.05). The soil organic carbon content of the three age groups, the total nitrogen content and alkali-hydrolyzable nitrogen content of the near-mature and over-aged plantations, and the total phosphorus and available phosphorus content of the over-aged plantation were significantly different between the 0-20 cm and 20-40 cm soil layers (P<0.05). These contents decreased with the deepening of soil layer. Correlation analysis showed that topographic factors, stand characteristics, and plant diversity were the factors affecting soil physical properties and nutrient changes in the P. massoniana plantations. Stepwise regression analysis showed that stand density and plant diversity were the main factors affecting soil physical properties, while topographic factors, stand characteristics, and plant diversity were the factors affecting soil nutrients. Redundancy analysis (RDA) showed that stand characteristics, plant diversity, and topographic factors explained 36.60%, 27.00% and 10.30% of the variation in the soil physicochemical properties, respectively.【Conclusion】 The plantation age has a significant impact on the soil nitrogen and phosphorus contents of P. massoniana plantations, suggesting that nitrogen fertilizer and phosphorus fertilizer should be added appropriately with the growth and development to maintain the productivity and sustainable development of P. massoniana plantations. Changes in the plantation age has no significant effect on soil physical properties, while the stand density and tree height are the main factors affecting the soil physical and chemical properties in P. massoniana plantations.
喀斯特 / 马尾松人工林 / 土壤理化性质 / 土壤养分 / 地形因子 / 林分特征 / 植物多样性
Karst / Pinus massoniana plantation / soil physical and chemical properties / soil nutrient / topographic factors / stand characteristics / plant diversity
[1] |
薛建辉, 周之栋, 吴永波. 喀斯特石漠化山地退化土壤生态修复研究进展[J]. 南京林业大学学报(自然科学版), 2022, 46(6):135-145.
|
[2] |
蔡磊, 杨健, 王六平, 等. 贵州省主要人工林近自然经营技术研究[J]. 林业实用技术, 2013(9):62-64.
|
[3] |
伍方骥, 刘娜, 胡培雷, 等. 典型喀斯特洼地植被恢复过程中土壤碳氮储量动态及其对极端内涝灾害的响应[J]. 中国生态农业学报(中英文), 2020, 28(3):429-437.
|
[4] |
吴平, 薛建辉. 典型喀斯特地区3种人工林对土壤理化和微生物特性的影响[J]. 南京林业大学学报(自然科学版), 2015, 39(5):67-72.
|
[5] |
曹洋, 徐娇, 谢冬冬. 基于文献计量的贵州喀斯特地区土壤养分特征研究[J]. 绿色科技, 2020(12):7-10,19.
|
[6] |
李鹏, 零天旺, 杨章旗, 等. 马尾松人工林林龄对土壤和叶片养分含量的影响[J]. 西北林学院学报, 2022, 37(5):9-16.
|
[7] |
戎宇. 喀斯特山地人工林凋落物对土壤肥力影响研究[D]. 南京: 南京林业大学, 2011.
|
[8] |
李鹏, 陈璇, 杨章旗, 等. 不同密度马尾松人工林枯落物输入对土壤理化性质的影响[J]. 水土保持学报, 2022, 36(2):368-377.
|
[9] |
舒韦维, 卢立华, 李华, 等. 林分密度对杉木人工林林下植被和土壤性质的影响[J]. 生态学报, 2021, 41(11):4521-4530.
|
[10] |
孙莉英, 栗清亚, 裴亮, 等. 地形因子对土壤理化性质和植物种类的影响[J]. 灌溉排水学报, 2020, 39(7):120-127.
|
[11] |
李鹏飞, 张兴昌, 郝明德, 等. 植被恢复对黄土高原矿区重构土壤理化性质、酶活性以及真菌群落的影响[J]. 水土保持通报, 2019, 39(5):1-7.
|
[12] |
徐雪蕾, 孙玉军, 周华, 等. 间伐强度对杉木人工林林下植被和土壤性质的影响[J]. 林业科学, 2019, 55(3):1-12.
|
[13] |
李歆玉, 徐林, 符裕红, 等. 喀斯特地区不同龄组马尾松人工林腐殖质化学计量特征研究[J]. 安徽农学通报, 2022, 28(10):81-83.
|
[14] |
雷丽群, 卢立华, 农友, 等. 不同林龄马尾松人工林土壤碳氮磷生态化学计量特征[J]. 林业科学研究, 2017, 30(6):954-960.
|
[15] |
刘小娥, 苏世平, 李毅. 兰州市南北两山典型灌丛土壤理化性质[J]. 草业学报, 2021, 30(6):28-39.
|
[16] |
寇江涛, 师尚礼, 王琦, 等. 垄沟集雨对紫花苜蓿草地土壤水分、容重和孔隙度的影响[J]. 中国生态农业学报, 2011, 19(6):1336-1342.
|
[17] |
鲍士旦. 土壤农化分析[M]. 3版. 北京: 中国农业出版社, 2000.
|
[18] |
张洋洋, 周清慧, 许骄阳, 等. 林龄对马尾松人工林林下植物与土壤种子库多样性的影响[J]. 生态环境学报, 2021, 30(11):2121-2129.
|
[19] |
崔宁洁, 张丹桔, 刘洋, 等. 不同林龄马尾松人工林林下植物多样性与土壤理化性质[J]. 生态学杂志, 2014, 33(10):2610-2617.
|
[20] |
许慧,
|
[21] |
杨志训, 秦连岗. 不同林龄马尾松人工林表层土壤养分特征分析[J]. 林业资源管理, 2014(3):101-104,121.
|
[22] |
马天舒, 丁伟林, 肖复明, 等. 不同年龄阶段陈山红心杉人工林土壤理化性质[J]. 中南林业科技大学学报, 2020, 40(12):114-124.
|
[23] |
盘金文, 郭其强, 孙学广, 等. 不同林龄马尾松人工林碳、氮、磷、钾养分含量及其生态化学计量特征[J]. 植物营养与肥料学报, 2020, 26(4):746-756.
|
[24] |
罗明霞, 胡宗达, 刘兴良, 等. 川西亚高山不同林龄粗枝云杉人工林土壤微生物生物量及酶活性[J]. 生态学报, 2021, 41(14):5632-5642.
|
[25] |
张沛健, 徐建民, 卢万鸿, 等. 雷州半岛不同林龄尾细桉人工林植物多样性和土壤理化性质分析[J]. 中南林业科技大学学报, 2021, 41(9):96-105.
|
[26] |
卢妮妮, 高志雄, 张鹏, 等. 杉木纯林土壤性质与林下植被的通径分析[J]. 东北林业大学学报, 2015, 43(7):73-77.
|
[27] |
李永强, 赵萌莉, 韩国栋, 等. 不同年限草原撂荒地土壤理化特性研究[J]. 中国草地学报, 2012, 34(3):61-64,69.
|
[28] |
秦晓佳, 丁贵杰. 不同林龄马尾松人工林土壤有机碳特征及其与养分的关系[J]. 浙江林业科技, 2012, 32(2):12-17.
|
[29] |
高孝威, 苏和, 白艳, 等. 不同林龄华北落叶松人工林林下植被与土壤理化特性变化特征[J]. 内蒙古林业科技, 2021, 47(2):10-14.
|
[30] |
肖欣, 王雄涛, 欧阳勋志. 马尾松人工林土壤有机碳特征及其与凋落物质量的关系[J]. 南京林业大学学报(自然科学版), 2015, 39(6):105-111.
|
[31] |
袁星明, 朱宁华, 郭耆, 等. 南亚热带不同人工林对土壤理化性质的影响及土壤质量评价[J]. 林业科学研究, 2022, 35(3):112-122.
|
[32] |
姜丽芳. 不同林分密度对杨树人工林生长及土壤理化性质的影响[J]. 安徽林业科技, 2022, 48(2):27-29.
|
[33] |
向玫. 不同林分密度对云杉人工林生长及土壤理化性质的影响[J]. 安徽林业科技, 2022, 48(1):25-27.
|
[34] |
郭弘婷, 纪小芳, 汪成, 等. 我国人工林林下灌木层植物多样性空间变异及影响要素[J]. 南京林业大学学报(自然科学版), 2022, 46(4): 144-152.
|
[35] |
龚益广, 徐明锋, 谢正生, 等. 杉木混交林的土壤生态化学计量及其林分结构影响因子研究[J]. 林业与环境科学, 2022, 38(1):18-27.
|
[36] |
黄瑞春, 朱宁华, 党鹏, 等. 石漠化地区不同人工林林下植物多样性及土壤理化性质[J]. 湖南林业科技, 2021, 48(4):10-17.
|
[37] |
杨家慧, 谭伟, 冯艳. 马尾松人工林土壤养分空间分布特征及其与地形因子的相关性分析[J]. 西南林业大学学报(自然科学), 2020, 40(4):23-29.
|
[38] |
董悦, 张永清, 刘彩彩. 晋中市土壤养分空间分布与影响因子的相关性[J]. 生态学报, 2018, 38(23):8621-8629.
|
/
〈 |
|
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