鄂中丘陵区不同龄组马尾松人工林矿物结合有机碳固存潜力

doi:10.11707/j.1001-7488.LYKX20260347

Abstract

Abstract:

Objective: This study aims to investigate the evolution patterns and driving factors of the effective saturation value and sequestration potential (defined as the percentage of the difference between the effective saturation value of actual mineral-associated organic carbon (MAOC) and its sequestration potential (the percentage of the difference between MAOC effective saturation value and actual content to effective saturation value) in Pinus massoniana plantations with stand development, so as to provide a scientific basis for carbon sink enhancement management. Method: P. massoniana plantations with different ages (young: 6 a, middle-aged: 13 a, near-mature: 29 a, mature: 38 a) in the hilly region of central Hubei Province were taken as the research object, and the plantations were subjected to a long-term field nutrient addition incubation experiment. The density-particle size fractionation method was used to quantify the dynamic changes of MAOC in the 0–10 cm soil layer of different age groups, evaluate the MAOC effective saturation value and sequestration potential, and identify the driving factors. Result: 1) Under natural conditions, the MAOC content in mature plantation (22.29±0.38 g·kg^–1) was significantly higher than that in near-mature (14.89±0.86 g·kg^–1), young (14.14±0.30 g·kg^?1), and middle-aged (11.82±0.69 g·kg^–1) plantations. 2) The MAOC effective saturation value in middle-aged plantation (19.29±0.55 g·kg^–1) was significantly lower than that in young (23.81±0.31 g·kg^–1) and mature (25.41±1.71 g·kg^–1) plantations. The MAOC sequestration potential significantly decreased with stand development, and had the lowest value observed in mature plantations 3) As soils approached MAOC saturation, the nitrogen and phosphorus contents in the mineral-associated fractions significantly increased across all age groups, while the C∶N and C∶P ratios significantly decreased. 4) The MAOC effective saturation value was primarily driven by the C∶P ratio of the mineral-associated fraction (R²=0.55, P<0.01), whereas soil specific surface area was the key factor determining the sequestration potential (R²=0.62, P<0.05). Conclusion: This study indicates that MAOC sequestration potential is highest in young plantations and lowest in mature plantations. In forest management, the long-term carbon sequestration function of P. massoniana plantations can be enhanced by quantitatively regulating soil nutrients to improve the C∶P ratio of the mineral-associated fraction.

Key words: Pinus massoniana plantation, age group, mineral-associated organic carbon, effective saturation value, sequestration potential

CLC Number:

S714.2

Jianwen Hu,Mengmeng Gou,Changfu Liu,Lixiong Zeng,Lei Lei,Jiajia Zhang,Wenfa Xiao. Mineral-Associated Organic Carbon Sequestration Potential of Pinus massoniana Plantations with Different Age Groups in the Hilly Region of Central Hubei[J]. Scientia Silvae Sinicae, 2026, 62(10): 30-41.

Figures/Tables 7

Table 1

Information of P. massoniana plantations with different ages"

项目Item	幼龄林 Young plantation	中龄林 Middle-aged plantation	近熟林 Near-mature plantation	成熟林 Mature plantation
相对位置Relative location	30°53′16″N, 112°55′42″E	30°54′40"N, 112°53′39″E	30°57′20″N 112°53′46″E	30°59′19″N, 112°56′4″E
海拔 Altitude/m	98.60±8.70	113.10±15.60	97.40±4.40	161.50±3.60
坡度 Slope/(°)	5	7	5	5
林木平均胸径 Mean diameter at breast height of trees/cm	7.20±0.10 C	10.76±0.29 C	23.63±1.19 B	30.08±1.51 A
平均树高 Mean tree height/m	6.7±0.1 C	8.2±0.1 C	12.2±0.4 B	15.4±0.2 A
林分密度 Stand density/(tree·hm^?2)	3 375±535 A	2 917±131 A	625±80 B	525±88 B
土壤密度 Soil density/(g·cm^?3)	1.26±0.07 A	1.31±0.02 A	1.36±0.03 A	1.19±0.06 A
黏粒含量 Clay content (< 2 μm) (%)	22.90±3.13 AB	21.72±0.27 AB	21.53±1.45 B	29.12±0.84 A
粉粒含量 Silt content (2–20 μm) (%)	66.17±2.12 A	65.44±1.01 AB	67.23±1.69 A	58.94±1.25 B
砂粒含量Sand content (> 20 μm) (%)	10.92±1.10 A	12.84±1.27 A	11.25±0.41 A	11.94±0.73 A
矿物颗粒含量Mineral grain content (< 53 μm) (%)	99.15±0.10 A	98.85±0.16 AB	98.93±0.10 AB	98.57±0.03 B
比表面积Specific surface area/(m²·g^?1)	80.92±4.40 A	71.69±4.12 AB	70.54±5.32 AB	54.48±3.01 B
pH	6.22±0.03 A	5.37±0.04 B	5.44±0.23 B	4.79±0.04 C
土壤有机碳含量 Soil organic carbon content/(g·kg^?1)	15.35±0.37 BC	13.22±0.83 C	18.28±1.05 ABC	21.9±1.07A
土壤全氮含量 Soil total nitrogen content/(g·kg^?1)	1.62±0.05 B	1.34±0.07 B	1.64±0.09 B	2.06±0.07 A
土壤全磷含量 Soil total phosphorus content/(mg·kg^?1)	227.21±60.84 A	326.47±8.74 A	278.13±31.97 A	292.63±8.19 A
游离态铁氧化物含量Free iron oxide content/(g·kg^?1)	0.74±0.05 C	1.15±0.07 B	1.02±0.09 BC	1.54±0.06 A
游离态铝氧化物含量 Free aluminum oxide content/(g·kg^?1)	2.62±0.36 B	3.17±0.38 B	3.63±0.45 AB	4.98±0.14 A
非晶形铁氧化物含量 Amorphous iron oxide content/(g·kg^?1)	3.51±0.26 AB	3.77±0.13 A	3.06±0.03 AB	2.88±0.12 B
非晶形铝氧化物含量 Amorphous aluminum oxide content/(g·kg^?1)	11.89±0.30 A	10.48±0.14 AB	9.55±0.45 B	9.24±0.57 B

Table 1

Fig.1

Table 2

Fig.2

Table 3

Fig.3

Table 4

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龄组 Age group	处理 Treatment	MAOC₀/ (g·kg^?1)	MAOC₅/ (g·kg^?1)	MAOC₆/ (g·kg^?1)	有效饱和值 Effective saturation value/(g·kg^?1)	饱和差 Saturation deficit/ (g·kg^?1)	固存潜力 Sequestration potential (%)
幼龄林 Young plantation	对照 Control	14.14±0.30 BCa	13.87±0.94 Ba	14.07±0.52 Ba	—	—	—
幼龄林 Young plantation	处理 Treatment	14.14±0.30 BCc	24.91±0.29 Aa	22.71±0.59 ABb	23.81±0.31 A	9.67±0.59 A	40.58±1.98 A

中龄林 Middle aged plantation	对照 Control	11.82±0.69 Ca	11.84±0.11 Ba	11.76±0.25 Ca	—	—	—
中龄林 Middle aged plantation	处理 Treatment	11.82±0.69 Cb	18.97±0.81 Aa	19.62±0.69 Ba	19.29±0.55 B	7.47±0.85 AB	38.67±3.79 A

近熟林 Near-mature plantation	对照 Control	14.89±0.86 Ba	13.22±0.91 Ba	11.79±0.53 Ca	—	—	—
近熟林 Near-mature plantation	处理 Treatment	14.89±0.86 Bb	22.02±0.73 Aa	21.95±1.15 ABa	21.98±0.24 AB	7.09±0.68 AB	32.32±3.36 A

成熟林 Mature plantation	对照 Control	22.29±0.38 Aa	21.93±1.53 Aa	22.79±0.16 Aa	—	—	—
成熟林 Mature plantation	处理 Treatment	22.29±0.38 Aa	24.80±2.45 Aa	26.03±1.76 Aa	25.41±1.71 A	3.12±2.09 B	11.34±6.98 B

指标Indicator	幼龄林 Young plantation	中龄林 Middle aged plantation	近熟林 Near-mature plantation	成熟林 Mature plantation
土壤含水量 Soil water content (%)	7.03±0.61 b	8.80±0.82 b	13.66±1.61 a	10.1±0.14 ab
土壤密度Soil density/(g·cm^?3)	0.99±0.01 a	1.00±0.03 a	1.01±0.03 a	1.00±0.01 a
矿物结合氮含量 Mineral-associated nitrogen content/(mg·g^?1)	2.86±0.05 a	2.29±0.04 b	2.56±0.05 ab	2.71±0.16 a
矿物结合磷含量 Mineral-associated phosphorus content/(mg·g^?1)	0.73±0.02 a	0.69±0.02 ab	0.60±0.02 b	0.60±0.04 b
矿物结合硫含量 Mineral-associated sulfur content/(mg·g^?1)	0.08±0.01 b	0.06±0.01 b	0.09±0.01 b	0.15±0.02 a
矿物结合组分碳氮比 Carbon-to-nitrogen ratio of the mineral-associated fraction	8.32±0.09 b	8.43±0.11 b	8.61±0.23 b	9.38±0.11 a
矿物结合组分碳磷比 Carbon-to-phosphorus ratio of the mineral-associated fraction	33.08±0.62 bc	28.14±1.19 c	36.69±1.39 b	43.15±1.97 a
矿物结合组分碳硫比Carbon-to-sulfur ratio of the mineral-associated fraction	314.12±39.78 ab	373.88±59.84 a	269.31±20.60 ab	182.05±30.02 b

逐步回归方程 Stepwise regression equation	决定系数 Determination coefficient	显著性 Significance
MAOC_sat = 0.345 6C∶P+10.4397	R²=0.55	P<0.01
CSP=0.942SSA?34.683	R²=0.62	P<0.05

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Mineral-Associated Organic Carbon Sequestration Potential of Pinus massoniana Plantations with Different Age Groups in the Hilly Region of Central Hubei

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