WANG Yueling,XU Hao,MAFan,et al.Soil Anti-scourability and Its Related Physical Properties on Typical Forestlands in Loess Hilly Region of Southern Ningxia[J].Research of Soil and Water Conservation,2021,28(01):37-43.
宁南黄土区典型林地土壤抗冲性及相关物理性质
- Title:
- Soil Anti-scourability and Its Related Physical Properties on Typical Forestlands in Loess Hilly Region of Southern Ningxia
- 文章编号:
- 1005-3409(2021)01-0037-07
- Keywords:
- loess hilly region of Southern Ningxia; artificial forest; soil hydro-physical properties; soil anti-scouribility
- 分类号:
- S157.1
- 文献标志码:
- A
- 摘要:
- 研究宁南黄土区典型林分类型土壤水文物理性质及抗冲性能,旨在从土壤抗冲性角度为该区域退耕还林工程的生态功能评价和树种配置提供科学依据。采用野外取样与室内试验相结合的方法,得到了4种林型(山杏纯林、山桃纯林、山杏×沙棘混交林、山杏×柠条混交林)的水文物理指标和土壤抗冲系数。结果表明:4种不同林型的土壤容重、总孔隙度、持水性能与抗冲系数存在显著差异。在0—30 cm土层,土壤容重随着土层深度的增加总体呈现递增的趋势,大小排序为山杏林×沙棘林>山杏林>山桃林>山杏×柠条林; 土壤总孔隙度和毛管孔隙度随土层的加深而减小,其中山杏×柠条混交林的含量最高; 最大持水量为山杏×沙棘林>山杏林>山桃林>山杏×柠条林,毛管持水量和田间持水量大小均为山杏×柠条林>山杏林>山桃林>山杏×沙棘林; 4种林型的土壤抗冲系数为山杏×柠条林>山杏×沙棘林>山杏林>山桃林。土壤容重与土壤总孔隙度、毛管持水量、田间持水量、抗冲系数均呈现极显著的负相关,土壤总孔隙度与土壤田间持水量、抗冲系数呈现极显著的正相关关系。其中以土壤总孔隙度与土壤田间持水量、抗冲系数的相关性最好。通过上述分析,总体表现出山杏×柠条混交林优于其他3种林型,能够有效改善土壤结构,提高土壤抗侵蚀性能。
- Abstract:
- In this study, we analyzed the soil hydro-physical properties and soil anti-scourability in typical forest types in the loess hilly region of Southern Ningxia in order to provide scientific basis for the ecological function evaluation and tree species allocation of the project of returning farmland to forest in the region from the perspective of soil anti-scourability. Soil hydro-physical indices and scourability coefficient of 4 forest types(pure forest of Prunus sibirica, pure forest of Prunus davidiana, mixed forest of Prunus sibirica×sea-buckthorn, mixed forest of Prunus sibirica×Caragana korshinskii)were obtained by the method of field sampling and laboratory test. The results showed that there were significant differences in soil bulk density, total porosity, water retention capacity and anti-scourability coefficient of 4 different forest types. In 0—30 cm soil layer, the soil bulk density showed an increasing trend with the increase of soil depth, and soil bulk density decreased in the order: Prunus sibirica×Hippophae rhamnoides forest>Prunus sibirica forest>Prunus davidiana forest>Prunus sibirica×Caragana korshinskii forest. The total porosity and capillary porosity of soil decreased with the depth of soil layer. The maximum water holding capacity decreased in the order: Prunus sibirica×Hippophae rhamnoides forest>Prunus sibirica forest>Prunus davidiana forest>Prunus sibirica×Caragana korshinskii forest. Both the gross water holding capacity and field water holding capacity decreased in the order: Prunus sibirica×Caragana korshinskii forest>Prunus davidiana forest>Prunus sibirica×Hippophae rhamnoides forest. The soil anti-scourability coefficients of 4 forest types decreased in the order: Prunus sibirica×Caragana korshinskii forest>mountain apricot×Hippophae rhamnoides forest>Prunus sibirica forest>Prunus davidiana forest. Soil bulk density was negatively correlated with soil total porosity, capillary water holding capacity, field water holding capacity and soil anti-scourability coefficient, while soil total porosity was positively correlated with soil water holding capacity and impact resistance coefficient. The correlation between soil total porosity and soil water holding capacity and soil resistance coefficient was the best. Based on the above analysis, it is concluded that Prunus sibirica×Caragana korshinskii mixed forest is superior to the other three forest types, which can effectively improve the soil structure and the soil erosion resistance ability.
参考文献/References:
[1] 傅伯杰.强化黄土高原土地利用水土保持效应[N].中国国土资源报,2016-09-22(6).
[2] 周正朝,上官周平.子午岭次生林植被演替过程的土壤抗冲性[J].生态学报,2006,26(10):3270-3275.
[3] 吴建平,韩新辉,任成杰,等.黄土丘陵区不同恢复年限退耕林地土壤碳氮差异及其影响因素[J].西北农林科技大学学报:自然科学版,2017,45(6):123-133.
[4] 赵允格,许明祥,王全九,等.黄土丘陵区退耕地生物结皮对土壤理化性状的影响[J].自然资源学报,2006,21(3):441-448.
[5] 李强,刘国彬,许明祥,等.黄土丘陵区撂荒地土壤抗冲性及相关理化性质[J].农业工程学报,2013,29(10):153-159.
[6] 李勇,徐晓琴,朱显谟,等.植物根系与土壤抗冲性[J].水土保持学报,1993,7(3):11-18.
[7] 张艺,李海光,余新晓,等.黄土高原典型流域土壤抗冲特性研究[J].水土保持通报,2012,32(2):60-63.
[8] 查小春,唐克丽.黄土丘陵林区开垦地土壤抗冲性的时间变化研究[J].水土保持通报,2001,21(2):8-11.
[9] 张建军,张宝颖,毕华兴,等.黄土区不同植被条件下的土壤抗冲性[J].北京林业大学学报,2004,26(6):25-29.
[10] 周佩华,郑世清,吴普特,等.黄土高原土壤抗冲性的试验研究[J].水土保持研究,1997,4(5):47-58,66.
[11] 王丹丹,张建军,丁杨,等.晋西黄土区退耕林地土壤抗冲性研究[J].水土保持学报,2014,28(3):14-18.
[12] 陈国靖.宁南黄土丘陵区土壤理化性质对不同植被恢复模式的响应[D].银川:宁夏大学,2018.
[13] 马璠.黄土丘陵区土壤抗冲性研究思考[M].银川:宁夏人民教育出版社,2019.
[14] 梁博,聂晓刚,杨东升,等.西藏尼洋河流域下游5种典型土地利用方式土壤物理性质差异分析[J].西北农林科技大学学报:自然科学版,2018,46(1):119-128.
[15] 李民义.晋西黄土区不同植被类型植物多样性及土壤水文物理特征研究[D].北京:北京林业大学,2013.
[16] 张晓梅,邸利,王彦辉,等.黄土高原典型林分土壤水文物理性质及持水性能[J].甘肃农业大学学报,2019,54(3):117-124,133.
[17] 顾宇书,邢兆凯,韩友志,等.浑河上游4种典型水源林土壤物理性质及其水源涵养功能[J].东北林业大学学报,2013,41(1):37-41.
[18] 鲁绍伟,毛富玲,靳芳,等.中国森林生态系统水源涵养功能[J].水土保持研究,2005,12(4):223-226.
[19] 韦洁.广西大青山人工纯林和混交林对植物多样性和土壤肥力的影响[D].南宁:广西大学,2011.
[20] 苏成西,尚宇南.不同退耕还林模式的土壤抗冲性研究[J].河南农业科学,2014,43(8):57-63.
[21] 邹文秀,韩晓增,陆欣春,等.不同土地利用方式对黑土剖面土壤物理性质的影响[J].水土保持学报,2015,29(5):187-193,199.
[22] 李超,周正朝,朱冰冰,等.黄土丘陵区不同撂荒年限土壤入渗及抗冲性研究[J].水土保持学报,2017,31(2):61-66.
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备注/Memo
收稿日期:2020-02-07 修回日期:2020-04-07
资助项目:国家重点研发计划课题“黄土梁状丘陵区林草植被体系结构优化及杏产业关键技术与示范”(2016YFC0501702); 宁夏回族自治区全产业链创新示范项目“宁夏多功能林业分区域研究与示范”(YES-12-16); 宁夏重点研发计划项目“宁夏黄土丘陵区小流域生态综合治理与高质量发展技术集成与示范”(2020BCF01001); 宁夏自然科学资助项目“宁南黄土区典型人工林生态系统群落多样性及土壤微生态效应”(2019AAC03289)
第一作者:王月玲(1980—),女,宁夏固原人,硕士,副研究员,主要从事黄土高原水土保持与生态环境建设研究。E-mail:wylnxnky@163.com