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Effects of Litter Decomposition on Soil N in Picea mongolica Forest at Different Forest Ages
In order to study the effects of litter decomposition on soil nitrogen of Piceamongolica in different forest ages, young forest (0–5a), middle-aged forest (5–30a), and near-mature forest (30–40a) stands were selected in the Baiyinaobao National Nature Reserve. Litter decomposition was assessed using the decomposition bag method. The seasonal and vertical spatial variation characteristics of total N, NH4+—N, and NO3−—N caused by litter decomposition in P. mongolica forest soil were studied for different stand ages. Results showed that: (1) There was a positive correlation between litter N content and soil organic matter, total N content, and NO3−—N content across different forest ages (p < 0.05). There was a negative correlation between litter N and NH4+—N contents. A negative correlation between litter C content and soil organic matter, total N, and NO3−—N contents was also observed. (2) In this study, the total N and NO3−—N increased with the increase in N content during litter decomposition.NH4+—N in the soil was positively correlated with sample date, soil NO3−—N, and forest age (p < 0.05), and negatively correlated with soil depth (p < 0.01). NO3−—N in the soil was negatively correlated with sample date and forest age (p < 0.05), and significantly negatively correlated with soil depth (p < 0.01). (3) the NH4+—N content is greater than that of NO3−—N in each soil layer for the three forest ages. The correlation analysis indicated which factors influenced NH4+—N and NO3−—N in the soil. The content decreased during February and November and increased in May and August. (4) The total N, NH4+—N, and NO3−—N in the forest soils across the three forest ages increased with the depth of the soil layer (0–50 cm) and showed an overall downward trend. The contents of NH4+—N in the soil layer from the young forest (0–10 cm, 10–20 cm and 20–30 cm, 30–40 cm, and 40–50 cm) differed significantly (p < 0.05), as did the NO3−—N results (p < 0.05), while results from the middle-aged forest and near-mature forest increased with soil layer depth. There was no significant difference in the NH4+—N soil content. (5) The NH4+—N in the forest soils showed a trend from mature forest > middle-aged forest > young forest. This trend for soil NO3−—N content is consistent with that of the NH4+—N content in the Picea mongolica forest soil.
Effects of Litter Decomposition on Soil N in Picea mongolica Forest at Different Forest Ages
In order to study the effects of litter decomposition on soil nitrogen of Piceamongolica in different forest ages, young forest (0–5a), middle-aged forest (5–30a), and near-mature forest (30–40a) stands were selected in the Baiyinaobao National Nature Reserve. Litter decomposition was assessed using the decomposition bag method. The seasonal and vertical spatial variation characteristics of total N, NH4+—N, and NO3−—N caused by litter decomposition in P. mongolica forest soil were studied for different stand ages. Results showed that: (1) There was a positive correlation between litter N content and soil organic matter, total N content, and NO3−—N content across different forest ages (p < 0.05). There was a negative correlation between litter N and NH4+—N contents. A negative correlation between litter C content and soil organic matter, total N, and NO3−—N contents was also observed. (2) In this study, the total N and NO3−—N increased with the increase in N content during litter decomposition.NH4+—N in the soil was positively correlated with sample date, soil NO3−—N, and forest age (p < 0.05), and negatively correlated with soil depth (p < 0.01). NO3−—N in the soil was negatively correlated with sample date and forest age (p < 0.05), and significantly negatively correlated with soil depth (p < 0.01). (3) the NH4+—N content is greater than that of NO3−—N in each soil layer for the three forest ages. The correlation analysis indicated which factors influenced NH4+—N and NO3−—N in the soil. The content decreased during February and November and increased in May and August. (4) The total N, NH4+—N, and NO3−—N in the forest soils across the three forest ages increased with the depth of the soil layer (0–50 cm) and showed an overall downward trend. The contents of NH4+—N in the soil layer from the young forest (0–10 cm, 10–20 cm and 20–30 cm, 30–40 cm, and 40–50 cm) differed significantly (p < 0.05), as did the NO3−—N results (p < 0.05), while results from the middle-aged forest and near-mature forest increased with soil layer depth. There was no significant difference in the NH4+—N soil content. (5) The NH4+—N in the forest soils showed a trend from mature forest > middle-aged forest > young forest. This trend for soil NO3−—N content is consistent with that of the NH4+—N content in the Picea mongolica forest soil.
Effects of Litter Decomposition on Soil N in Picea mongolica Forest at Different Forest Ages
Yunchao Liu (author) / Lixin Chen (author) / Wenbiao Duan (author) / Yongan Bai (author) / Xiaolan Li (author)
2022
Article (Journal)
Electronic Resource
Unknown
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