Eurasian Soil Science - The results are presented of modeling the “contour water flooding” biotechnology aimed at cleaning heavily petroleum-polluted agrosoddy-podzolic soils (Albic... 相似文献
Journal of Soils and Sediments - Phytolith-occluded carbon (PhytOC) is mainly derived from the products of photosynthesis, which can be preserved in soils and sediments for hundreds-to-thousands of... 相似文献
Nitrogen (N) is an important nutrient for re-vegetation during ecosystem restoration, but the effects of cover restoration on soil N transformations are not fully understood. This study was conducted to investigate N transformations in soils with different cover restoration ages in Eastern China.
Materials and methods
Soil samples were collected from four degraded and subsequently restored lands with restoration ages of 7, 17, 23, and 35 years along with an adjacent control of degraded land. A 15N tracing technique was used to quantify gross N transformation rates.
Results and discussion
Compared with degraded land, soil organic carbon (SOC) and total N (TN) increased by 1.60–3.97 and 2.49–5.36 times in restoration land. Cover restoration increased ammonium and nitrate immobilization, and dissimilatory nitrate reduction to ammonium (DNRA) by 0.56–0.96, 0.34–2.10, and 0.79–3.45 times, respectively, indicating that restoration was beneficial for N retention. There were positive correlations between SOC content and ammonium and nitrate immobilization and DNRA, indicating that the increase in soil N retention capacity may be ascribed to increasing SOC concentrations. The stimulating effect of SOC on ammonium immobilization was greater than its effect on organic N mineralization, so while SOC and TN increased, inorganic N supply did not increase. Autotrophic and heterotrophic nitrification increased with increasing SOC and TN concentrations. Notably, heterotrophic nitrification was an important source of NO3??N production, accounting for 47–67% of NO3??N production among all restoration ages.
Conclusions
The capacity of N retention was improved by cover restoration, leading to an increase in soil organic carbon and total N over time, but inorganic N supply capacity did not change with cover restoration age.
Journal of Soils and Sediments - Organic manure is beneficial for macro-aggregate formation and soil organic carbon (SOC), but how SOC change in aggregate fractions in time-series is still... 相似文献
为探究不同施肥和保水措施对油茶土壤N_2O排放的影响,采用静态暗箱-气相色谱法,设置对照(B0CK)、氮肥(N,0.13 g N·kg~(-1))、磷肥(P,0.065 g P·kg~(-1))、氮磷肥(NP,0.13 g N·kg~(-1)+0.065 g P·kg~(-1))、低复合保水材料(生物炭和聚丙烯酰胺,B1,每盆13.65 g炭+1.35 g聚丙烯酰胺)、高复合保水材料(生物炭和聚丙烯酰胺,B2,每盆27.30 g炭+2.70 g聚丙烯酰胺)、低复合保水材料和N(NB1)、高复合保水材料和N(NB2)、低复合保水材料和P(PB1)、高复合保水材料和P(PB2)、低复合保水材料和NP(NPB1)、高复合保水材料和NP(NPB2),共12个处理,进行不同施肥和保水措施下土壤N_2O排放的差异比较。结果表明,N、P添加均显著增加土壤N_2O的累积排放量,NP添加与对照无差异。施加复合保水材料抑制土壤N_2O的排放,随着复合保水材料施用量的增加,土壤N_2O的排放显著降低,与对照相比,B1和B2处理N_2O减排50%以上。N添加条件下,与对照相比,添加复合保水材料NB1、NB2的N_2O累积排放显著降低。P与复合保水材料无交互作用。N、P和复合保水材料对土壤N_2O累积排放量具有显著作用,在NP同施时,与对照相比,添加复合保水材料NPB1、NPB2的N_2O累积排放分别降低了1.18%、30.69%。因此,高复合保水材料类型的施肥措施对减少油茶土壤N_2O排放具有重要意义,从而对缓解全球气候变化具有重要影响。 相似文献