水蚀作用下红壤丘陵区土壤特性的空间分异特征

doi:10.12302/j.issn.1000-2006.202204052

国家林草科技领军期刊
中国精品科技期刊
中国高校百佳科技期刊
江苏省新闻出版政府奖期刊奖
RCCSE林学权威期刊（A+）
CSCD核心期刊
Scopus数据库收录期刊
中文核心期刊
SCD核心期刊

作者加群：102861116

微信公众号：南京林业大学学报

高级检索

南京林业大学学报（自然科学版） ›› 2023, Vol. 47 ›› Issue (6): 77-84.doi: 10.12302/j.issn.1000-2006.202204052

所属专题：山水林田湖草一体化保护和生态修复——土壤侵蚀修复研究

• 专题报道Ⅱ：山水林田湖草一体化保护和生态修复——土壤侵蚀修复研究（执行主编张金池） • 上一篇下一篇

水蚀作用下红壤丘陵区土壤特性的空间分异特征

张相¹(), 丁鸣鸣², 林杰¹^,^*(), 李卓远¹, 崔琳琳¹, 郭赓¹, 杨皓¹

1.南京林业大学林草学院、水土保护学院,南方现代林业协同创新中心,江苏省水土保持与生态修复重点实验室,江苏南京 210037
2.南京市水务局,江苏南京 210036

收稿日期:2022-04-21 修回日期:2022-06-17 出版日期:2023-11-30 发布日期:2023-11-23
通讯作者: *林杰(jielin@njfu.edu.cn),教授。
基金资助:
国家自然科学基金面上项目(31870600)

Spatial differentiation of soil properties in hilly red soil region under water erosion

ZHANG Xiang¹(), DING Mingming², LIN Jie¹^,^*(), LI Zhuoyuan¹, CUI Linlin¹, GUO Geng¹, YANG Hao¹

1. College of Forestry and Grassland, College of Soil and Water Conservation, Co-Innovation Center for Sustainable Forestry in Southern China, Jiangsu Province Key Laboratory of Soil and Water Conservation and Ecological Restoration, Nanjing Forestry University, Nanjing 210037,China
2. Nanjing Water Affairs Bureau, Nanjing 210036,China

Received:2022-04-21 Revised:2022-06-17 Online:2023-11-30 Published:2023-11-23

摘要/Abstract

摘要：

【目的】揭示由水蚀引起的土壤质量变异的规律,为南方红壤丘陵区水土流失防治及低效林改造提供科学性的数据支撑。【方法】选取江西省吉安市青原山小流域作为南方红壤丘陵区的典型区,按照典型性和代表性将小流域划分坡位,对各坡位土壤团聚体组成进行分析,并应用相关性分析探究水蚀过程中各指标间的影响关系。【结果】水力侵蚀改变了土壤容重和土壤孔隙的空间分布格局,致使侵蚀区的土壤抗蚀性变弱,沉积区影响不大,加速了土壤侵蚀的发生。长期侵蚀后土壤容重增大,与其他坡位相比,坡脚处土壤容重显著增加了0.16 g/cm³(P<0.05),而饱和持水量和毛管孔隙度均表现为显著减小(P<0.05);水蚀后,土壤质地的组成也发生了变化,土壤砂粒含量显著增加,黏粒和粉粒含量显著减小(P<0.05)。水蚀过程对不同坡位的土壤养分影响不一,侵蚀后坡上、坡中和坡下土壤全氮、速效磷、有机碳含量和碳氮比降低,坡上各养分含量显著降低(P<0.05);与侵蚀前相比,侵蚀后坡脚处的养分含量均增加,速效磷显著增加了39.31%(P<0.05)。水蚀后不同坡位的水稳性团聚体质量分数(R_0.25)、平均质量直径(MWD)和几何平均直径(GMD)均呈现降低的变化,坡脚处的变化不明显,土壤结构稳定性最高。【结论】南方红壤丘陵区生态系统脆弱,长期水蚀作用可使红壤的团聚体稳定性降低,水蚀过程使侵蚀-沉积部位的土壤理化性质发生了空间分异,植被覆盖度和枯落物厚度是主要的环境影响因素。

关键词: 土壤侵蚀, 水蚀作用, 理化性质, 团聚体, 空间分异, 南方红壤丘陵区

Abstract:

【Objective】This study aims to reveale the law of soil quality variation caused by water erosion provides scientific data support for soil erosion control and low-efficiency forest transformation in hilly red soil region of southern china.【Method】The small watershed of Qingyuan Mountain in Ji ’an City, Jiangxi Province was selected as a typical area of red soil hilly area in southern China. According to the typicality and representativeness, the small watershed was divided into slope positions, and three sections were set up to collect soil repeatedly. The composition of soil aggregates was analyzed, and the correlation analysis was used to explore the relationship between various indicators in the process of water erosion.【Result】Water erosion changed the spatial distribution pattern of bulk density and soil porosity, resulting in weaker soil anti-erodibility in erosion area and less influence in deposition area, which accelerated the occurrence of soil erosion. Soil bulk density increased after long-term erosion. Compared with other slope positions, soil bulk density at slope toe increased significantly by 0.16 g/cm³ (P < 0.05), while saturated water holding capacity and capillary porosity decreased significantly (P < 0.05). After water erosion, the composition of soil texture also changed, soil sand content increased significantly, clay and silt content decreased significantly (P < 0.05). The water erosion process had different effects on soil nutrients at different slope positions. The soil total nitrogen, available phosphorus, organic carbon content and carbon-nitrogen ratio decreased on the upper, middle and lower slopes, and the content on the slope decreased significantly (P < 0.05). Compared with other slope positions, the nutrient content at the toe of the slope increased, and the available phosphorus increased significantly by 39.31% (P < 0.05). After water erosion, the mass fraction (R_0.25), mean mass diameter (MWD) and geometric mean diameter (GMD) of water-stable aggregates at different slope positions showed a decreasing trend, and the change at the foot of the slope was not obvious, and the stability of soil structure was the highest.【Conclusion】The ecosystem of red soil hilly area in southern China is fragile. Long-term water erosion can reduce the stability of red soil aggregates. The water erosion process causes spatial differentiation of soil physical and chemical properties in erosion-deposition sites. Vegetation coverage and litter thickness are the main environmental factors.

Key words: soil erosion, water erosion, physicochemical properties, aggregates, spatial differentiation, red soil hilly area in southern China

中图分类号:

S714.2

张相,丁鸣鸣,林杰,等. 水蚀作用下红壤丘陵区土壤特性的空间分异特征[J]. 南京林业大学学报（自然科学版）, 2023, 47(6): 77-84.

ZHANG Xiang, DING Mingming, LIN Jie, LI Zhuoyuan, CUI Linlin, GUO Geng, YANG Hao. Spatial differentiation of soil properties in hilly red soil region under water erosion[J].Journal of Nanjing Forestry University (Natural Science Edition), 2023, 47(6): 77-84.DOI: 10.12302/j.issn.1000-2006.202204052.

图/表 7

图1

表1

表2

图2

图3

表3

图4

参考文献 30

[1]	ASMAMAW L, MOHAMMED A, MATHIAS T. Predicting soil erosion by water:rusle application for soil conservation planning in central rift valley of Ethiopia[J]. Environ Eng Manag J, 2021, 20(9):1521-1534.DOI:10.30638/eemj.2021.141.
[2]	LAL R. Soil erosion and the global carbon budget[J]. Environ Int, 2003, 29(4):437-450.DOI:10.1016/S0160-4120(02)00192-7.
[3]	史志华, 宋长青. 土壤水蚀过程研究回顾[J]. 水土保持学报, 2016, 30(5):1-10.
	SHI Z H, SONG C Q. Water erosion processes:a historical review[J]. J Soil Water Conserv, 2016, 30(5):1-10.DOI:10.13870/j.cnki.stbcxb.2016.05.001.
[4]	林杰, 张相, 姜姜, 等. 水力侵蚀过程中土壤有机碳循环研究进展[J]. 南京林业大学学报(自然科学版), 2022, 46(6): 187-194.
	LIN J, ZHANG X, JIANG J, et al. A review on the soil organic carbon cycling under water erosion[J]. J Nanjing For Univ (Nat Sci Ed), 2022, 46(6): 187-194.DOI: 10.12302/j.issn.1000-2006.202206017.
[5]	聂小东. 水力侵蚀对红壤丘陵区土壤有机碳迁移分布及稳定机制的影响[D]. 长沙: 湖南大学, 2017.
	NIE X D. Effects of water erosion on the mechanisms of soil organic carbon migration,redistribution and stability in the red soil hilly region[D]. Changsha: Hunan University, 2017.
[6]	WANG H, ZHAO W W, JIA L Z. Progress and prospect of soil water erosion research over past decade based on the bibliometrics analysis[J]. Sci Soil Water Conserv, 2021, 19(1):141-151.
[7]	周咪, 肖海兵, 聂小东, 等. 近30年国内外土壤有机碳研究进程解析与展望[J]. 水土保持研究, 2020, 27(3):391-400.
	ZHOU M, XIAO H B, NIE X D, et al. Analysis and prospect of soil organic carbon research process in recent 30 years at home and abroad[J]. Res Soil Water Conserv, 2020, 27(3):391-400.DOI:10.13869/j.cnki.rswc.2020.03.056.
[8]	DAI Q H, PENG X D, WANG P J, et al. Surface erosion and underground leakage of yellow soil on slopes in Karst regions of southwest China[J]. Land Degrad Dev, 2018, 29(8):2438-2448.DOI:10.1002/ldr.2960.
[9]	LU J, ZHENG F L, LI G F, et al. The effects of raindrop impact and runoff detachment on hillslope soil erosion and soil aggregate loss in the Mollisol region of northeast China[J]. Soil Tillage Res, 2016, 161:79-85.DOI:10.1016/j.still.2016.04.002.
[10]	王占礼, 邵明安. 黄土坡地耕作侵蚀对土壤养分影响的研究[J]. 农业工程学报, 2002, 18(6):63-67.
	WANG Z L, SHAO M A. Effects of tillage erosion on soil nutrients in loess sloping land of China[J]. Trans Chin Soc Agric Eng, 2002, 18(6):63-67.
[11]	李奕, 满秀玲, 蔡体久, 等. 大兴安岭山地樟子松天然林土壤水分物理性质及水源涵养功能研究[J]. 水土保持学报, 2011, 25(2):87-91,96.
	LI Y, MAN X L, CAI T J, et al. Research on physical properties of soil moisture and water conservation of Scotch pine forest in Da Xing’an Mountains[J]. J Soil Water Conserv, 2011, 25(2):87-91,96.DOI:10.13870/j.cnki.stbcxb.2011.02.009.
[12]	贺小容, 何丙辉, 秦伟, 等. 不同坡长条件下扰动地表对土壤养分的影响[J]. 水土保持学报, 2013, 27(5):154-158,163.
	HE X R, HE B H, QIN W, et al. Effect of disturbance surface on soil nutrient under different slope length[J]. J Soil Water Conserv, 2013, 27(5):154-158,163.DOI:10.13870/j.cnki.stbcxb.2013.05.020.
[13]	张合兵, 聂小军, 程静霞. ¹³⁷Cs示踪采煤沉陷坡土壤侵蚀及其对土壤养分的影响[J]. 农业工程学报, 2015, 31(4):137-143.
	ZHANG H B, NIE X J, CHENG J X. ¹³⁷Cs tracing of soil erosion and its impact on soil nutrients across subsidence slope induced by coal mining[J]. Trans Chin Soc Agric Eng, 2015, 31(4):137-143.DOI:10.3969/j.issn.1002-6819.2015.04.020.
[14]	赵鑫, 翟胜, 李建豹, 等. 不同坡位条件对毛乌素沙地长柄扁桃林地土壤水分的影响[J]. 水土保持通报, 2020, 40(4):45-52.
	ZHAO X, ZHAI S, LI J B, et al. Effects of different slope conditions on soil moisture of Amygdalus pedunculate woodland in Muus sandy land[J]. Bull Soil Water Conserv, 2020, 40(4):45-52.DOI:10.13961/j.cnki.stbctb.2020.04.007.
[15]	苏子龙, 张光辉, 于艳. 典型黑土区农业小流域不同坡向和坡位的土壤水分变化特征[J]. 中国水土保持科学, 2013, 11(6):39-44.
	SU Z L, ZHANG G H, YU Y. Variation of soil moisture with slope aspect and position in a small agricultural watershed in the typical black soil region[J]. Sci Soil Water Conserv, 2013, 11(6):39-44.DOI:10.16843/j.sswc.2013.06.007.
[16]	田迅, 高凯, 张丽娟, 等. 坡位对土壤水分及植被空间分布的影响[J]. 水土保持通报, 2015, 35(5):12-16.
	TIAN X, GAO K, ZHANG L J, et al. Effects of slope position on spatial distribution of soil water and vegetation in sandy land[J]. Bull Soil Water Conserv, 2015, 35(5):12-16.DOI:10.13961/j.cnki.stbctb.2015.05.068.
[17]	张相, 李肖, 林杰, 等. 南方红壤丘陵区侵蚀沟道内土壤团聚体及有机碳特征[J]. 农业工程学报, 2020, 36(19):115-123.
	ZHANG X, LI X, LIN J, et al. Characteristics of soil aggregates and organic carbon in eroded gully in red soil region of southern China[J]. Trans Chin Soc Agric Eng, 2020, 36(19):115-123.
[18]	吉增宝. 用数码照片和Photoshop计算植被覆盖度的简易方法[J]. 水土保持应用技术, 2015(5):10-11.
	JI Z B. Simple method of calculating vegetation coverage by digital photos and Photoshop[J]. Technol Soil Water Conserv, 2015(5):10-11.
[19]	鲁如坤. 土壤农业化学分析方法[M]. 北京: 中国农业科技出版社, 2000.
	LU R K. Agricultural chemical analysis method of soil[M]. Beijing: China Agriculture Scientech Press, 2000.
[20]	林杰, 张阳, 朱艳芳, 等. 淮北土石山区不同土地利用方式对土壤团聚体组成的影响[J]. 中国农业科技导报, 2019, 21(4):133-142.
	LIN J, ZHANG Y, ZHU Y F, et al. Effects of different land use types on soil aggregate composition in rocky mountain area of northern Huai River[J]. J Agric Sci Technol, 2019, 21(4):133-142.DOI:10.13304/j.nykjdb.2018.0207.
[21]	邹鑫, 陈春峰, 刘文杰. 西双版纳橡胶种植对土壤团聚体及理化性质的影响[J]. 土壤通报, 2020, 51(3):597-605.
	ZOU X, CHEN C F, LIU W J. Effects of rubber plantation on soil aggregate stability and physicochemical properties in Xishuangbanna[J]. Chin J Soil Sci, 2020, 51(3):597-605.DOI:10.19336/j.cnki.trtb.2020.03.13.
[22]	刘强, 穆兴民, 高鹏, 等. 土壤水力侵蚀对土壤质量理化指标影响的研究综述[J]. 水土保持研究, 2020, 27(6):386-392.
	LIU Q, MU X M, GAO P, et al. Review of studies on the effects of soil water erosion on physical and chemical properties of soil quality[J]. Res Soil Water Conserv, 2020, 27(6):386-392.DOI:10.13869/j.cnki.rswc.2020.06.049.
[23]	冯志珍, 郑粉莉, 易祎. 薄层黑土微生物生物量碳氮对土壤侵蚀—沉积的响应[J]. 土壤学报, 2017, 54(6):1332-1344.
	FENG Z Z, ZHENG F L, YI Y. Responses of microbial biomass carbon and nitrogen to erosion and deposition in black soil thin in depth[J]. Acta Pedol Sin, 2017, 54(6):1332-1344.DOI:10.11766/trxb201703080015.
[24]	钱婧, 张丽萍, 王文艳. 红壤坡面土壤团聚体特性与侵蚀泥沙的相关性[J]. 生态学报, 2018, 38(5):1590-1599.
	QIAN J, ZHANG L P, WANG W Y. The relationship between soil aggregates and eroded sediments from sloping vegetated red soils of south China[J]. Acta Ecol Sin, 2018, 38(5):1590-1599.DOI:10.5846/stxb201611112299.
[25]	黄尚书, 钟义军, 黄欠如, 等. 耕作深度及培肥方式对红壤坡耕地土壤理化性质及作物产量的影响[J]. 中国土壤与肥料, 2020(4):72-83.
	HUANG S S, ZHONG Y J, HUANG Q R, et al. Effects of tillage depths and fertilizing patterns on soil physical-chemical properties and crop yield in red soil slop field[J]. Soil Fertil Sci China, 2020(4):72-83.DOI:10.11838/sfsc.1673-6257.19308.
[26]	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.
	SUN L Y, LI Q Y, PEI L, et al. Effects of topographic factors on soil physical and chemical properties and plant species[J]. J Irrigation Drainage, 2020, 39(7):120-127.DOI:10.13522/j.cnki.ggps.2020119.
[27]	李浙华, 李生宇, 李丙文, 等. 不同植被覆盖度沙垄土壤化学性质的空间分异[J]. 干旱区研究, 2020, 37(1):160-167.
	LI Z H, LI S Y, LI B W, et al. Spatial variation of soil chemical properties of longitudinal dunes with different vegetation coverage levels[J]. Arid Zone Res, 2020, 37(1):160-167.DOI:10.13866/j.azr.2020.01.18.
[28]	石璞, CHIAHUE D Y, 赵鹏志. 间歇性降雨对土壤团聚体粒级及磷、铜、锌富集的影响[J]. 土壤学报, 2021, 58(4):948-956.
	SHI P, CHIAHUE D Y, ZHAO P Z. Effect of intermittent rainfall on size distribution and phosphorus,copper and zinc enrichment of soil aggregates[J]. Acta Pedol Sin, 2021, 58(4):948-956.
[29]	李肖, 陈晨, 林杰, 等. 侵蚀强度对淮北土石山区土壤团聚体组成及稳定性的影响[J]. 水土保持研究, 2019, 26(4):56-61,67.
	LI X, CHEN C, LIN J, et al. Effect of erosion intensity on composition and stability of soil aggregates in rocky mountain area of Huaibei[J]. Res Soil Water Conserv, 2019, 26(4):56-61,67.DOI:10.13869/j.cnki.rswc.2019.04.009.
[30]	胡亚鲜, NIKOLAUS J K. 利用土壤颗粒的沉降粒级研究泥沙的迁移与分布规律[J]. 土壤学报, 2017, 54(5):1115-1124.
	HU Y X, NIKOLAUS J K. Using settling velocity to investigate the patterns of sediment transport and deposition[J]. Acta Pedol Sin, 2017, 54(5):1115-1124.DOI:10.11766/trxb201703100056.

取样地点(代号) sampling site (code)	海拔/m altitude	平均坡度/ (°) mean slope	枯落物厚度/cm litter thickness	植被覆盖度/% forest and grass coverage	¹³⁷Cs含量/ (Bq·m^-2) ¹³⁷Cs content	土壤侵蚀模数/ (t·km^-2·a^-1) soil erosion modulu	区划 sectional division
坡上upper slope(US)	132.61	3.75	2.4	30.79	4 288.21	-3 440.15	沉积区
坡中middle slope(MS)	107.47	30.96	1.4	26.96	824.57	2 591.18	侵蚀区
坡下down slope(DS)	78.52	12.78	1.8	25.53	1 149.66	887.52	侵蚀区
坡脚toe slope(TS)	65.09	28.28	2.1	16.72	845.02	3 166.87	侵蚀区

取样地点 sampling site	组别 group	容重/ (g·cm^-3) BD	c(砂粒)/%	c(粉粒)/%	c(黏粒)/%	饱和持水量/% WHC	毛管孔隙度/% CAP
坡上 US	侵蚀前	1.26±0.10 a	12.98±0.70 a	77.56±0.33 a	9.46±1.03 a	36.26±1.00 a	34.89±1.07 a
	侵蚀后	1.27±0.07 a	35.58±0.32 b	63.30±0.36 b	1.12±0.11 b	19.48±0.51 b	31.92±0.59b
坡中 MS	侵蚀前	0.97±0.09 a	13.29±1.55 a	80.20±0.86 a	6.51±0.69 a	39.29±1.14 a	36.56±0.65 a
	侵蚀后	0.99±0.06 a	51.17±0.38 b	46.86±0.33 b	1.97±0.06 b	24.96±2.09 b	29.17±1.76 b
坡下 DS	侵蚀前	1.41±0.02 a	14.58±7.47 a	77.41±5.99 a	8.01±1.49 a	32.81±0.11 a	37.5±0.64 a
	侵蚀后	1.43±0.11 a	53.04±0.97 b	44.79±1.03 b	2.14±0.03 b	23.46±2.08 b	34.21±0.70 b
坡脚 TS	侵蚀前	0.91±0.02 a	3.98±0.04 a	91.51±0.51 a	4.51±0.47 a	71.09±4.96 a	57.37±2.48 a
	侵蚀后	1.07±0.06 b	51.37±0.70 b	46.75±0.70 b	1.88±0.05 b	40.56±2.05 b	43.48±1.41 b

取样地点 sampling site	R_0.25/%		平均质量直径/mm MWD		几何平均直径/mm GMD
取样地点 sampling site	CK	T	CK	T	CK	T
坡上US	86.34±0.51 a	81.93±0.73 b	1.57±0.01 a	1.42±0.01 b	0.62±0.01 a	0.56±0.01 b
坡中MS	67.47±5.61 a	61.36±1.23 a	1.13±0.12 a	0.97±0.01 a	0.34±0.08 a	0.31±0.01 a
坡下DS	80.55±4.80 a	62.42±1.14 b	1.45±0.11 a	0.97±0.01 b	0.53±0.08 a	0.29±0.01 b
坡脚TS	64.23±2.30 a	63.84±0.85 a	1.09±0.01 a	1.11±0.01 a	0.32±0.02 a	0.32±0.01 a

水蚀作用下红壤丘陵区土壤特性的空间分异特征

Spatial differentiation of soil properties in hilly red soil region under water erosion

RichHTML

PDF

可视化

摘要/Abstract

引用本文

使用本文

图/表 7

参考文献 30

相关文章 15

编辑推荐

Metrics

本文评价

作者

读者

审稿

[1]	杨瑞, 吴朝明, 朱骊, 胡海波. 苏南丘陵区坡面经济林土壤侵蚀特征[J]. 南京林业大学学报（自然科学版）, 2023, 47(6): 70-76.
[2]	王苗苗, 王恩姮, 韩明钊, 李永江, 玉苏普. 基于Le Bissonnais法研究有机物料对黑土团聚体稳定性的影响[J]. 南京林业大学学报（自然科学版）, 2023, 47(4): 191-199.
[3]	贺坤, 王俊洁, 王本耀, 朱海军, 奉树成. 上海市行道树土壤肥力特征及其空间分布[J]. 南京林业大学学报（自然科学版）, 2023, 47(3): 164-172.
[4]	林杰, 张相, 姜姜, 蒯杰, 郭赓, 孟苗婧, 李肖. 水力侵蚀过程中土壤有机碳循环研究进展[J]. 南京林业大学学报（自然科学版）, 2022, 46(6): 187-194.
[5]	李惠芝, 关庆伟, 赵家豪, 李俊杰, 王磊, 李凤凤, 左兴平, 陈斌. 地形对麻栎人工林土壤肥力质量的影响[J]. 南京林业大学学报（自然科学版）, 2022, 46(5): 161-168.
[6]	陈超, 齐斐, 徐雁南, 黎家作, 赵传普, 苏新宇. 基于空间自相关的县域尺度土壤侵蚀抽样方法研究[J]. 南京林业大学学报（自然科学版）, 2022, 46(3): 177-184.
[7]	刘倩倩, 彭孝楠, 刘鑫, 王舒甜, 戴康龙, 徐海兵, 董丽娜, 张金池. 踩踏干扰下紫金山土壤质量季节变化特征[J]. 南京林业大学学报（自然科学版）, 2022, 46(3): 185-193.
[8]	刘珂, 李明阳, 李灵, 田康, 樊亚男, 王志刚, 瞿明凯, 黄标. 南水北调中线工程水源地土壤有机碳密度空间分异及驱动因素研究[J]. 南京林业大学学报（自然科学版）, 2022, 46(2): 35-43.
[9]	朱家琪, 满秀玲, 王飞. 寒温带4种森林类型土壤团聚体有机碳氮特征[J]. 南京林业大学学报（自然科学版）, 2021, 45(5): 71-83.
[10]	王冰, 张鹏杰, 张秋良. 不同林型兴安落叶松林土壤团聚体及其有机碳特征[J]. 南京林业大学学报（自然科学版）, 2021, 45(3): 15-24.
[11]	王瑞, 王国兵, 徐瑾, 徐晓. 凋落物与蚯蚓对杨树人工林土壤团聚体分布及其碳氮含量的影响[J]. 南京林业大学学报（自然科学版）, 2021, 45(3): 25-29.
[12]	王爱斌, 宋慧芳, 张流洋, 张明, 杨诗雯, 张凌云. 生物肥和菌肥对蓝莓苗生长及土壤养分的影响[J]. 南京林业大学学报（自然科学版）, 2020, 44(6): 63-70.
[13]	王国兵,王瑞,徐瑾,曹国华,阮宏华. 生物炭对杨树人工林土壤微生物生物量碳、氮、磷及其化学计量特征的影响[J]. 南京林业大学学报（自然科学版）, 2019, 62(02): 1-6.
[14]	王潇,胡海波,施海新. 稻壳炭改良盐渍土性状研究[J]. 南京林业大学学报（自然科学版）, 2019, 62(01): 193-197.
[15]	刘国华,方正,郑笑,范婷婷,高佳伟,王福升,张金池. 全国14个竹产区毛竹竹炭理化性质分析[J]. 南京林业大学学报（自然科学版）, 2018, 61(06): 13-19.