干旱区研究 ›› 2024, Vol. 41 ›› Issue (8): 1354-1363.doi: 10.13866/j.azr.2024.08.09 cstr: 32277.14.AZR.20240809
董鹏1(), 任悦1, 高广磊1,2,3,4,5(
), 丁国栋1,3,4,5, 张英1,3,4,5
收稿日期:
2024-01-10
修回日期:
2024-05-27
出版日期:
2024-08-15
发布日期:
2024-08-22
通讯作者:
高广磊. E-mail: gaoguanglei@bjfu.edu.cn作者简介:
董鹏(1997-),硕士研究生,主要研究方向为荒漠生态学. E-mail: DDB820650@bjfu.edu.cn
基金资助:
DONG Peng1(), REN Yue1, GAO Guanglei1,2,3,4,5(
), DING Guodong1,3,4,5, ZHANG Ying1,3,4,5
Received:
2024-01-10
Revised:
2024-05-27
Published:
2024-08-15
Online:
2024-08-22
摘要:
为了揭示呼伦贝尔沙地樟子松(Pinus sylvestris var. mongolica)枯落物和土壤C、N、P化学计量特征及其主要驱动因素。以不同龄组(中龄林、近熟林、成熟林)樟子松人工林和天然林为研究对象,分析枯落物和土壤C、N、P化学计量特征,并探究其与土壤因子间的相关关系。结果表明:(1) 分解程度显著影响枯落物C、N、P和C:N(P<0.05),土层显著影响土壤N、C:N、C:P(P<0.05),林龄及其与分解程度、土层的交互作用对枯落物和土壤C、N、P化学计量特征无显著影响(P>0.05)。天然林与人工林枯落物和土壤C、N含量和C:P、N:P存在显著差异(P<0.05)。(2) 枯落物C含量与枯落物N、P含量呈显著正相关(P<0.05),枯落物C:P与C:N呈显著正相关(P<0.05);土壤C:P与土壤N:P、C:N呈显著正相关(P<0.05)。(3) 枯落物C、N、P化学计量特征主要受pH、磷酸酶和脲酶的显著影响(P<0.05),土壤C、N、P化学计量特征主要受pH、磷酸酶和转化酶的显著影响(P<0.05)。呼伦贝尔沙地樟子松林生长可能受氮限制,而枯落物分解可能受磷限制;枯落物和土壤C、N、P化学计量特征的主要驱动因子分别为pH和磷酸酶。研究结果对樟子松人工林经营管理具有指导意义。
董鹏, 任悦, 高广磊, 丁国栋, 张英. 呼伦贝尔沙地樟子松枯落物和土壤碳、氮、磷化学计量特征[J]. 干旱区研究, 2024, 41(8): 1354-1363.
DONG Peng, REN Yue, GAO Guanglei, DING Guodong, ZHANG Ying. Stoichiometry of carbon, nitrogen, and phosphorus in the litter and soil of Pinus sylvestris var. mongolica in the Hulunbuir Sandy Land[J]. Arid Zone Research, 2024, 41(8): 1354-1363.
表4
樟子松人工林双因素方差分析"
F(P) | |||||||
---|---|---|---|---|---|---|---|
C | N | P | C:N | C:P | N:P | ||
枯落物 | 林龄 | 0.416(0.870) | 3.292(0.175) | 4.635(0.175) | 0.494(0.635) | 15.650(0.026) | 4.455(0.126) |
分解程度 | 166.630(<0.001) | 4. 221(0.016) | 5.959(0.01) | 7.272(0.001) | 1.367(0.277) | 1.231(0.320) | |
林龄×分解程度 | 1.67(0.193) | 0.28(0.839) | 0.09(0.966) | 0.375(0.772) | 0.17(0.916) | 0.40(0.752) | |
土壤 | 林龄 | 0.366(0.721) | 3.612(0.159) | 32.990(0.009) | 1.424(0.367) | 3.435(0.168) | 0.538(0.631) |
土层 | 2.720(0.067) | 25.138(<0.001) | 0. 188(0.903) | 41.503(<0.001) | 10.465(<0.001) | 1.629(0.209) | |
林龄×土层 | 4.89(0.007) | 3.20(0.037) | 0.344(0.794) | 0.7(0.559) | 1.83(0.162) | 1.63(0.202) |
表5
枯落物、土壤C、N、P化学计量特征与土壤因子间的皮尔逊分析"
土壤因子 | C | N | P | C:N | C:P | N:P | |
---|---|---|---|---|---|---|---|
枯落物 | SWC | -0.163 | -0.24 | -0.3 | 0.027 | 0.202 | 0.206 |
NO3- | -0.233 | 0.013 | -0.13 | -0.274 | 0.006 | 0.194 | |
pH | -0.107 | -0.505** | -0.637** | 0.383* | 0.646** | 0.424** | |
AP | -0.02 | -0.109 | 0.029 | 0.084 | -0.035 | -0.119 | |
INV | 0.078 | 0.208 | 0.238 | -0.102 | -0.16 | -0.109 | |
URE | 0.488** | 0.3 | 0.350* | 0.276 | 0.049 | -0.151 | |
PHO | 0.639** | 0.515** | 0.362* | 0.256 | 0.138 | -0.033 | |
PRO | 0.362* | 0.192 | 0.251 | 0.247 | 0.027 | -0.166 | |
土壤 | SWC | 0.187 | 0.395* | 0.211 | -0.098 | -0.166 | -0.155 |
NO3- | -0.288 | -0.228 | 0.142 | 0.187 | -0.072 | -0.174 | |
pH | 0.071 | -0.13 | -0.163 | 0.447** | 0.259 | -0.221 | |
AP | 0.042 | -0.083 | -0.274 | 0.085 | 0.187 | 0.048 | |
INV | -0.213 | -0.352* | -0.116 | 0.097 | 0.176 | 0.246 | |
URE | 0.132 | 0.212 | -0.083 | 0.152 | 0.284 | 0.435** | |
PHO | 0.273 | 0.446** | 0.073 | 0.111 | 0.352* | 0.527** | |
PRO | 0.068 | 0.350* | 0.014 | 0.165 | 0.087 | 0.342* |
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